Po-Plain-GU-Boundaries

fid fid geologicUnitId geologicUnitIdentifier inspireId_localId InspireId_namespace geologicUnitDescription geologicUnitName geologicUnitType boundId boundaryName contactType geologicUnitId1 material1 role1 material2 role2 eventProcess olderNamedAge youngerNamedAge depthASL depthASL_uom thickness thickness_uom
Po-Plain-GU-Boundaries.1 1 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -540.9 m m
Po-Plain-GU-Boundaries.2 2 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -326.4 m m
Po-Plain-GU-Boundaries.3 3 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -319.9 m m
Po-Plain-GU-Boundaries.4 4 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -319.9 m m
Po-Plain-GU-Boundaries.5 5 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -319.9 m m
Po-Plain-GU-Boundaries.6 6 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -319.9 m m
Po-Plain-GU-Boundaries.7 7 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -319.9 m m
Po-Plain-GU-Boundaries.8 8 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -320.0 m m
Po-Plain-GU-Boundaries.9 9 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -322.1 m m
Po-Plain-GU-Boundaries.10 10 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -310.7 m m
Po-Plain-GU-Boundaries.11 11 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -292.2 m m
Po-Plain-GU-Boundaries.12 12 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -273.3 m m
Po-Plain-GU-Boundaries.13 13 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -269.8 m m
Po-Plain-GU-Boundaries.14 14 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -259.5 m m
Po-Plain-GU-Boundaries.15 15 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -256.4 m m
Po-Plain-GU-Boundaries.16 16 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -257.5 m m
Po-Plain-GU-Boundaries.17 17 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -260.9 m m
Po-Plain-GU-Boundaries.18 18 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -262.6 m m
Po-Plain-GU-Boundaries.19 19 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -264.9 m m
Po-Plain-GU-Boundaries.20 20 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -268.6 m m
Po-Plain-GU-Boundaries.21 21 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -271.0 m m
Po-Plain-GU-Boundaries.22 22 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -271.3 m m
Po-Plain-GU-Boundaries.23 23 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -278.0 m m
Po-Plain-GU-Boundaries.24 24 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -282.7 m m
Po-Plain-GU-Boundaries.25 25 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -288.5 m m
Po-Plain-GU-Boundaries.26 26 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -306.5 m m
Po-Plain-GU-Boundaries.27 27 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -329.6 m m
Po-Plain-GU-Boundaries.28 28 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -336.5 m m
Po-Plain-GU-Boundaries.29 29 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -291.4 m m
Po-Plain-GU-Boundaries.30 30 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -262.7 m m
Po-Plain-GU-Boundaries.31 31 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -244.8 m m
Po-Plain-GU-Boundaries.32 32 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -241.9 m m
Po-Plain-GU-Boundaries.33 33 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -257.1 m m
Po-Plain-GU-Boundaries.34 34 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -245.2 m m
Po-Plain-GU-Boundaries.35 35 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -254.7 m m
Po-Plain-GU-Boundaries.36 36 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -285.6 m m
Po-Plain-GU-Boundaries.37 37 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -316.8 m m
Po-Plain-GU-Boundaries.38 38 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -348.3 m m
Po-Plain-GU-Boundaries.39 39 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -380.0 m m
Po-Plain-GU-Boundaries.40 40 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -405.5 m m
Po-Plain-GU-Boundaries.41 41 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -406.3 m m
Po-Plain-GU-Boundaries.42 42 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -410.2 m m
Po-Plain-GU-Boundaries.43 43 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -414.1 m m
Po-Plain-GU-Boundaries.44 44 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -418.2 m m
Po-Plain-GU-Boundaries.45 45 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -422.0 m m
Po-Plain-GU-Boundaries.46 46 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -423.1 m m
Po-Plain-GU-Boundaries.47 47 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -414.5 m m
Po-Plain-GU-Boundaries.48 48 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -405.5 m m
Po-Plain-GU-Boundaries.49 49 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -406.3 m m
Po-Plain-GU-Boundaries.50 50 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -409.7 m m
Po-Plain-GU-Boundaries.51 51 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -410.7 m m
Po-Plain-GU-Boundaries.52 52 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -693.8 m m
Po-Plain-GU-Boundaries.53 53 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -469.7 m m
Po-Plain-GU-Boundaries.54 54 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.1 m m
Po-Plain-GU-Boundaries.55 55 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.1 m m
Po-Plain-GU-Boundaries.56 56 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.1 m m
Po-Plain-GU-Boundaries.57 57 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.1 m m
Po-Plain-GU-Boundaries.58 58 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.1 m m
Po-Plain-GU-Boundaries.59 59 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.1 m m
Po-Plain-GU-Boundaries.60 60 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.1 m m
Po-Plain-GU-Boundaries.61 61 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.1 m m
Po-Plain-GU-Boundaries.62 62 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.63 63 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.64 64 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.65 65 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.66 66 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.67 67 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.68 68 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.1 m m
Po-Plain-GU-Boundaries.69 69 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.70 70 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.71 71 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.72 72 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.73 73 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.74 74 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.75 75 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.76 76 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.77 77 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.78 78 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.79 79 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.80 80 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.81 81 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.82 82 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.83 83 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.84 84 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.85 85 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.86 86 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.87 87 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.88 88 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.89 89 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.90 90 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.91 91 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.92 92 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.93 93 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.94 94 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.95 95 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.96 96 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.1 m m
Po-Plain-GU-Boundaries.97 97 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.1 m m
Po-Plain-GU-Boundaries.98 98 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.99 99 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.100 100 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.101 101 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.102 102 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.103 103 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.104 104 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.105 105 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.1 m m
Po-Plain-GU-Boundaries.106 106 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.1 m m
Po-Plain-GU-Boundaries.107 107 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.1 m m
Po-Plain-GU-Boundaries.108 108 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.1 m m
Po-Plain-GU-Boundaries.109 109 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.1 m m
Po-Plain-GU-Boundaries.110 110 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.1 m m
Po-Plain-GU-Boundaries.111 111 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.1 m m
Po-Plain-GU-Boundaries.112 112 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.1 m m
Po-Plain-GU-Boundaries.113 113 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.1 m m
Po-Plain-GU-Boundaries.114 114 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.115 115 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.1 m m
Po-Plain-GU-Boundaries.116 116 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 3.1 m m
Po-Plain-GU-Boundaries.117 117 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.6 m m
Po-Plain-GU-Boundaries.118 118 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1377.0 m m
Po-Plain-GU-Boundaries.119 119 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1485.4 m m
Po-Plain-GU-Boundaries.120 120 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1485.9 m m
Po-Plain-GU-Boundaries.121 121 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1486.3 m m
Po-Plain-GU-Boundaries.122 122 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1486.8 m m
Po-Plain-GU-Boundaries.123 123 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1487.3 m m
Po-Plain-GU-Boundaries.124 124 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1478.9 m m
Po-Plain-GU-Boundaries.125 125 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1479.3 m m
Po-Plain-GU-Boundaries.126 126 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1479.8 m m
Po-Plain-GU-Boundaries.127 127 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1480.3 m m
Po-Plain-GU-Boundaries.128 128 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1480.7 m m
Po-Plain-GU-Boundaries.129 129 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1478.9 m m
Po-Plain-GU-Boundaries.130 130 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1428.0 m 1141.0 m
Po-Plain-GU-Boundaries.131 131 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1402.3 m 1067.5 m
Po-Plain-GU-Boundaries.132 132 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1383.7 m 1008.6 m
Po-Plain-GU-Boundaries.133 133 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1679.9 m m
Po-Plain-GU-Boundaries.134 134 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1717.7 m m
Po-Plain-GU-Boundaries.135 135 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1736.7 m m
Po-Plain-GU-Boundaries.136 136 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1662.0 m m
Po-Plain-GU-Boundaries.137 137 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1653.7 m m
Po-Plain-GU-Boundaries.138 138 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1652.5 m m
Po-Plain-GU-Boundaries.139 139 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1651.3 m m
Po-Plain-GU-Boundaries.140 140 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1650.2 m m
Po-Plain-GU-Boundaries.141 141 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1649.0 m m
Po-Plain-GU-Boundaries.142 142 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1647.8 m m
Po-Plain-GU-Boundaries.143 143 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1646.6 m m
Po-Plain-GU-Boundaries.144 144 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1645.5 m m
Po-Plain-GU-Boundaries.145 145 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1644.3 m m
Po-Plain-GU-Boundaries.146 146 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1643.4 m m
Po-Plain-GU-Boundaries.147 147 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1642.3 m m
Po-Plain-GU-Boundaries.148 148 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1641.1 m m
Po-Plain-GU-Boundaries.149 149 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1639.9 m m
Po-Plain-GU-Boundaries.150 150 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1638.8 m m
Po-Plain-GU-Boundaries.151 151 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1637.6 m m
Po-Plain-GU-Boundaries.152 152 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1629.9 m m
Po-Plain-GU-Boundaries.153 153 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1581.6 m m
Po-Plain-GU-Boundaries.154 154 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1646.2 m m
Po-Plain-GU-Boundaries.155 155 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1742.6 m m
Po-Plain-GU-Boundaries.156 156 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1719.7 m m
Po-Plain-GU-Boundaries.157 157 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1719.3 m m
Po-Plain-GU-Boundaries.158 158 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1718.8 m m
Po-Plain-GU-Boundaries.159 159 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1719.1 m m
Po-Plain-GU-Boundaries.160 160 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1718.5 m m
Po-Plain-GU-Boundaries.161 161 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1718.0 m m
Po-Plain-GU-Boundaries.162 162 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1717.4 m m
Po-Plain-GU-Boundaries.163 163 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1716.9 m m
Po-Plain-GU-Boundaries.164 164 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1716.3 m m
Po-Plain-GU-Boundaries.165 165 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1715.8 m m
Po-Plain-GU-Boundaries.166 166 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1708.3 m m
Po-Plain-GU-Boundaries.167 167 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1707.8 m m
Po-Plain-GU-Boundaries.168 168 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1707.3 m m
Po-Plain-GU-Boundaries.169 169 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1706.7 m m
Po-Plain-GU-Boundaries.170 170 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1706.2 m m
Po-Plain-GU-Boundaries.171 171 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1705.6 m m
Po-Plain-GU-Boundaries.172 172 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1705.1 m m
Po-Plain-GU-Boundaries.173 173 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1704.5 m m
Po-Plain-GU-Boundaries.174 174 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1704.8 m m
Po-Plain-GU-Boundaries.175 175 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1704.3 m m
Po-Plain-GU-Boundaries.176 176 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1703.7 m m
Po-Plain-GU-Boundaries.177 177 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1703.2 m m
Po-Plain-GU-Boundaries.178 178 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1704.5 m m
Po-Plain-GU-Boundaries.179 179 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1705.8 m m
Po-Plain-GU-Boundaries.180 180 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1707.1 m m
Po-Plain-GU-Boundaries.181 181 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1708.4 m m
Po-Plain-GU-Boundaries.182 182 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1700.9 m m
Po-Plain-GU-Boundaries.183 183 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1702.2 m m
Po-Plain-GU-Boundaries.184 184 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1703.5 m m
Po-Plain-GU-Boundaries.185 185 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1704.8 m m
Po-Plain-GU-Boundaries.186 186 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1706.1 m m
Po-Plain-GU-Boundaries.187 187 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1707.4 m m
Po-Plain-GU-Boundaries.188 188 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1708.7 m m
Po-Plain-GU-Boundaries.189 189 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1710.8 m m
Po-Plain-GU-Boundaries.190 190 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1712.1 m m
Po-Plain-GU-Boundaries.191 191 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1713.4 m m
Po-Plain-GU-Boundaries.192 192 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1714.7 m m
Po-Plain-GU-Boundaries.193 193 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1716.0 m m
Po-Plain-GU-Boundaries.194 194 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1553.1 m m
Po-Plain-GU-Boundaries.195 195 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1476.4 m 817.2 m
Po-Plain-GU-Boundaries.196 196 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1597.2 m 836.1 m
Po-Plain-GU-Boundaries.197 197 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1719.2 m 857.2 m
Po-Plain-GU-Boundaries.198 198 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1743.6 m 856.0 m
Po-Plain-GU-Boundaries.199 199 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1811.9 m 894.0 m
Po-Plain-GU-Boundaries.200 200 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1968.1 m 926.2 m
Po-Plain-GU-Boundaries.201 201 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1969.4 m 927.4 m
Po-Plain-GU-Boundaries.202 202 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1970.8 m 928.6 m
Po-Plain-GU-Boundaries.203 203 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1972.1 m 929.9 m
Po-Plain-GU-Boundaries.204 204 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1973.5 m 931.1 m
Po-Plain-GU-Boundaries.205 205 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1977.1 m 934.7 m
Po-Plain-GU-Boundaries.206 206 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.4 m 935.9 m
Po-Plain-GU-Boundaries.207 207 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.4 m m
Po-Plain-GU-Boundaries.208 208 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.4 m 935.8 m
Po-Plain-GU-Boundaries.209 209 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.4 m m
Po-Plain-GU-Boundaries.210 210 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.4 m 935.7 m
Po-Plain-GU-Boundaries.211 211 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.6 m m
Po-Plain-GU-Boundaries.212 212 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.6 m m
Po-Plain-GU-Boundaries.213 213 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.6 m 935.7 m
Po-Plain-GU-Boundaries.214 214 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.6 m m
Po-Plain-GU-Boundaries.215 215 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.6 m 935.5 m
Po-Plain-GU-Boundaries.216 216 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.0 m m
Po-Plain-GU-Boundaries.217 217 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.0 m 944.8 m
Po-Plain-GU-Boundaries.218 218 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.0 m 944.7 m
Po-Plain-GU-Boundaries.219 219 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.0 m m
Po-Plain-GU-Boundaries.220 220 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.0 m 944.6 m
Po-Plain-GU-Boundaries.221 221 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.0 m m
Po-Plain-GU-Boundaries.222 222 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.7 m 945.2 m
Po-Plain-GU-Boundaries.223 223 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.7 m m
Po-Plain-GU-Boundaries.224 224 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.7 m m
Po-Plain-GU-Boundaries.225 225 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.7 m 945.0 m
Po-Plain-GU-Boundaries.226 226 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.7 m m
Po-Plain-GU-Boundaries.227 227 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.9 m 945.1 m
Po-Plain-GU-Boundaries.228 228 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.9 m m
Po-Plain-GU-Boundaries.229 229 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.9 m m
Po-Plain-GU-Boundaries.230 230 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.9 m 944.9 m
Po-Plain-GU-Boundaries.231 231 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.9 m 944.8 m
Po-Plain-GU-Boundaries.232 232 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.9 m 944.8 m
Po-Plain-GU-Boundaries.233 233 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.9 m 944.7 m
Po-Plain-GU-Boundaries.234 234 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1988.4 m 944.2 m
Po-Plain-GU-Boundaries.235 235 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1982.4 m m
Po-Plain-GU-Boundaries.236 236 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1982.3 m m
Po-Plain-GU-Boundaries.237 237 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1982.1 m m
Po-Plain-GU-Boundaries.238 238 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1981.9 m m
Po-Plain-GU-Boundaries.239 239 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1981.7 m m
Po-Plain-GU-Boundaries.240 240 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1981.6 m m
Po-Plain-GU-Boundaries.241 241 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1981.4 m m
Po-Plain-GU-Boundaries.242 242 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1981.2 m m
Po-Plain-GU-Boundaries.243 243 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1981.1 m m
Po-Plain-GU-Boundaries.244 244 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1980.9 m m
Po-Plain-GU-Boundaries.245 245 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1980.7 m m
Po-Plain-GU-Boundaries.246 246 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1980.5 m m
Po-Plain-GU-Boundaries.247 247 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1980.4 m m
Po-Plain-GU-Boundaries.248 248 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1980.2 m m
Po-Plain-GU-Boundaries.249 249 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1980.0 m m
Po-Plain-GU-Boundaries.250 250 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1979.8 m m
Po-Plain-GU-Boundaries.251 251 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1979.7 m m
Po-Plain-GU-Boundaries.252 252 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1979.5 m m
Po-Plain-GU-Boundaries.253 253 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.5 m 929.0 m
Po-Plain-GU-Boundaries.254 254 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.3 m 928.5 m
Po-Plain-GU-Boundaries.255 255 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1978.1 m 928.1 m
Po-Plain-GU-Boundaries.256 256 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1977.9 m 927.7 m
Po-Plain-GU-Boundaries.257 257 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1977.8 m 927.2 m
Po-Plain-GU-Boundaries.258 258 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1977.7 m 926.9 m
Po-Plain-GU-Boundaries.259 259 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1977.6 m 926.5 m
Po-Plain-GU-Boundaries.260 260 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1898.4 m 800.7 m
Po-Plain-GU-Boundaries.261 261 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1794.8 m 759.2 m
Po-Plain-GU-Boundaries.262 262 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1752.3 m 712.3 m
Po-Plain-GU-Boundaries.263 263 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1753.9 m 718.9 m
Po-Plain-GU-Boundaries.264 264 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1626.5 m 657.8 m
Po-Plain-GU-Boundaries.265 265 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1598.7 m 692.8 m
Po-Plain-GU-Boundaries.266 266 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1495.1 m 716.7 m
Po-Plain-GU-Boundaries.267 267 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1318.5 m 703.0 m
Po-Plain-GU-Boundaries.268 268 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -197.3 m m
Po-Plain-GU-Boundaries.269 269 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -197.3 m m
Po-Plain-GU-Boundaries.270 270 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -197.3 m m
Po-Plain-GU-Boundaries.271 271 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -197.3 m m
Po-Plain-GU-Boundaries.272 272 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -197.3 m m
Po-Plain-GU-Boundaries.273 273 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -197.3 m m
Po-Plain-GU-Boundaries.274 274 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -197.3 m m
Po-Plain-GU-Boundaries.275 275 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -197.3 m m
Po-Plain-GU-Boundaries.276 276 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -197.3 m m
Po-Plain-GU-Boundaries.277 277 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -197.3 m m
Po-Plain-GU-Boundaries.278 278 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -197.3 m m
Po-Plain-GU-Boundaries.279 279 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -917.9 m m
Po-Plain-GU-Boundaries.280 280 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -826.2 m m
Po-Plain-GU-Boundaries.281 281 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -785.9 m m
Po-Plain-GU-Boundaries.282 282 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -754.6 m m
Po-Plain-GU-Boundaries.283 283 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -720.2 m m
Po-Plain-GU-Boundaries.284 284 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -686.6 m m
Po-Plain-GU-Boundaries.285 285 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -664.2 m m
Po-Plain-GU-Boundaries.286 286 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -663.1 m m
Po-Plain-GU-Boundaries.287 287 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -662.1 m m
Po-Plain-GU-Boundaries.288 288 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -661.0 m m
Po-Plain-GU-Boundaries.289 289 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -660.0 m m
Po-Plain-GU-Boundaries.290 290 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -757.5 m m
Po-Plain-GU-Boundaries.291 291 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -71.4 m 8.1 m
Po-Plain-GU-Boundaries.292 292 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -71.4 m 3.7 m
Po-Plain-GU-Boundaries.293 293 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -71.4 m 0.6 m
Po-Plain-GU-Boundaries.294 294 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -71.4 m 5.0 m
Po-Plain-GU-Boundaries.295 295 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -71.4 m 9.3 m
Po-Plain-GU-Boundaries.296 296 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -71.4 m 13.6 m
Po-Plain-GU-Boundaries.297 297 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.6 m m
Po-Plain-GU-Boundaries.298 298 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 2.3 m m
Po-Plain-GU-Boundaries.299 299 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 3.3 m m
Po-Plain-GU-Boundaries.300 300 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.301 301 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.3 m m
Po-Plain-GU-Boundaries.302 302 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -0.5 m m
Po-Plain-GU-Boundaries.303 303 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian 0.0 m m
Po-Plain-GU-Boundaries.304 304 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2.5 m 8.5 m
Po-Plain-GU-Boundaries.305 305 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -441.0 m 275.2 m
Po-Plain-GU-Boundaries.306 306 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -581.5 m 406.3 m
Po-Plain-GU-Boundaries.307 307 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -689.4 m 546.2 m
Po-Plain-GU-Boundaries.308 308 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -691.6 m 548.5 m
Po-Plain-GU-Boundaries.309 309 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -698.7 m 511.0 m
Po-Plain-GU-Boundaries.310 310 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -509.9 m 100.0 m
Po-Plain-GU-Boundaries.311 311 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1019.4 m 166.6 m
Po-Plain-GU-Boundaries.312 312 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1165.4 m 325.3 m
Po-Plain-GU-Boundaries.313 313 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -978.2 m m
Po-Plain-GU-Boundaries.314 314 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -900.3 m m
Po-Plain-GU-Boundaries.315 315 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -796.0 m m
Po-Plain-GU-Boundaries.316 316 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1150.1 m m
Po-Plain-GU-Boundaries.317 317 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1155.0 m m
Po-Plain-GU-Boundaries.318 318 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1160.0 m m
Po-Plain-GU-Boundaries.319 319 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1165.0 m m
Po-Plain-GU-Boundaries.320 320 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1170.1 m m
Po-Plain-GU-Boundaries.321 321 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1281.2 m m
Po-Plain-GU-Boundaries.322 322 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -921.1 m 325.3 m
Po-Plain-GU-Boundaries.323 323 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -911.6 m 500.1 m
Po-Plain-GU-Boundaries.324 324 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -909.4 m 499.3 m
Po-Plain-GU-Boundaries.325 325 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -907.2 m 498.4 m
Po-Plain-GU-Boundaries.326 326 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -903.8 m 496.5 m
Po-Plain-GU-Boundaries.327 327 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -900.5 m 494.5 m
Po-Plain-GU-Boundaries.328 328 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -897.2 m 492.6 m
Po-Plain-GU-Boundaries.329 329 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -893.9 m 490.6 m
Po-Plain-GU-Boundaries.330 330 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -890.5 m 488.7 m
Po-Plain-GU-Boundaries.331 331 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -610.1 m 191.1 m
Po-Plain-GU-Boundaries.332 332 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -618.8 m 181.4 m
Po-Plain-GU-Boundaries.333 333 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -646.5 m 191.3 m
Po-Plain-GU-Boundaries.334 334 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -586.3 m 98.3 m
Po-Plain-GU-Boundaries.335 335 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -514.7 m m
Po-Plain-GU-Boundaries.336 336 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -482.9 m m
Po-Plain-GU-Boundaries.337 337 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -480.8 m m
Po-Plain-GU-Boundaries.338 338 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -533.5 m m
Po-Plain-GU-Boundaries.339 339 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -535.9 m m
Po-Plain-GU-Boundaries.340 340 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -538.4 m m
Po-Plain-GU-Boundaries.341 341 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -595.6 m m
Po-Plain-GU-Boundaries.342 342 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -837.3 m 172.3 m
Po-Plain-GU-Boundaries.343 343 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -912.3 m 140.5 m
Po-Plain-GU-Boundaries.344 344 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -997.3 m 258.7 m
Po-Plain-GU-Boundaries.345 345 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -980.5 m 295.8 m
Po-Plain-GU-Boundaries.346 346 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -884.2 m 198.6 m
Po-Plain-GU-Boundaries.347 347 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -706.9 m 114.3 m
Po-Plain-GU-Boundaries.348 348 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -707.2 m 103.2 m
Po-Plain-GU-Boundaries.349 349 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -836.5 m 193.2 m
Po-Plain-GU-Boundaries.350 350 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -799.2 m 175.8 m
Po-Plain-GU-Boundaries.351 351 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -801.5 m 199.2 m
Po-Plain-GU-Boundaries.352 352 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -827.6 m 231.0 m
Po-Plain-GU-Boundaries.353 353 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -952.4 m 285.8 m
Po-Plain-GU-Boundaries.354 354 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -952.8 m 285.7 m
Po-Plain-GU-Boundaries.355 355 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -953.2 m 285.7 m
Po-Plain-GU-Boundaries.356 356 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -953.6 m 285.7 m
Po-Plain-GU-Boundaries.357 357 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -954.0 m 285.6 m
Po-Plain-GU-Boundaries.358 358 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -954.4 m 285.6 m
Po-Plain-GU-Boundaries.359 359 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -954.7 m 285.5 m
Po-Plain-GU-Boundaries.360 360 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -955.1 m 285.5 m
Po-Plain-GU-Boundaries.361 361 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -955.5 m 285.5 m
Po-Plain-GU-Boundaries.362 362 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -955.9 m 285.4 m
Po-Plain-GU-Boundaries.363 363 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1005.9 m 253.4 m
Po-Plain-GU-Boundaries.364 364 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1001.2 m 243.8 m
Po-Plain-GU-Boundaries.365 365 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -995.3 m 239.6 m
Po-Plain-GU-Boundaries.366 366 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -989.4 m 235.5 m
Po-Plain-GU-Boundaries.367 367 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -983.5 m 231.3 m
Po-Plain-GU-Boundaries.368 368 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -978.3 m 227.9 m
Po-Plain-GU-Boundaries.369 369 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -972.4 m m
Po-Plain-GU-Boundaries.370 370 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1290.4 m 553.5 m
Po-Plain-GU-Boundaries.371 371 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1806.5 m 1125.8 m
Po-Plain-GU-Boundaries.372 372 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1788.7 m m
Po-Plain-GU-Boundaries.373 373 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1787.8 m m
Po-Plain-GU-Boundaries.374 374 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1786.9 m 1115.1 m
Po-Plain-GU-Boundaries.375 375 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1786.0 m 1114.1 m
Po-Plain-GU-Boundaries.376 376 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1785.2 m 1113.1 m
Po-Plain-GU-Boundaries.377 377 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1784.3 m m
Po-Plain-GU-Boundaries.378 378 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1783.4 m m
Po-Plain-GU-Boundaries.379 379 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1782.6 m m
Po-Plain-GU-Boundaries.380 380 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1781.7 m 1109.1 m
Po-Plain-GU-Boundaries.381 381 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1772.1 m 1099.4 m
Po-Plain-GU-Boundaries.382 382 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1771.2 m m
Po-Plain-GU-Boundaries.383 383 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1770.3 m m
Po-Plain-GU-Boundaries.384 384 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1692.0 m 1079.9 m
Po-Plain-GU-Boundaries.385 385 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1570.4 m m
Po-Plain-GU-Boundaries.386 386 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1568.5 m m
Po-Plain-GU-Boundaries.387 387 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1485.5 m 831.2 m
Po-Plain-GU-Boundaries.388 388 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1484.5 m 830.0 m
Po-Plain-GU-Boundaries.389 389 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1483.4 m 828.7 m
Po-Plain-GU-Boundaries.390 390 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1482.4 m 827.4 m
Po-Plain-GU-Boundaries.391 391 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1481.3 m 826.2 m
Po-Plain-GU-Boundaries.392 392 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1480.3 m 824.9 m
Po-Plain-GU-Boundaries.393 393 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1479.2 m 823.7 m
Po-Plain-GU-Boundaries.394 394 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1478.2 m 822.4 m
Po-Plain-GU-Boundaries.395 395 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1477.1 m 821.1 m
Po-Plain-GU-Boundaries.396 396 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1476.5 m 820.3 m
Po-Plain-GU-Boundaries.397 397 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1475.5 m 819.0 m
Po-Plain-GU-Boundaries.398 398 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1474.4 m 817.8 m
Po-Plain-GU-Boundaries.399 399 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1473.4 m 816.5 m
Po-Plain-GU-Boundaries.400 400 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1472.3 m 815.3 m
Po-Plain-GU-Boundaries.401 401 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1471.3 m 814.0 m
Po-Plain-GU-Boundaries.402 402 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1432.8 m 766.2 m
Po-Plain-GU-Boundaries.403 403 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1184.3 m m
Po-Plain-GU-Boundaries.404 404 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -996.5 m 361.6 m
Po-Plain-GU-Boundaries.405 405 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -995.9 m 361.3 m
Po-Plain-GU-Boundaries.406 406 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -995.4 m 361.0 m
Po-Plain-GU-Boundaries.407 407 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -994.8 m 360.7 m
Po-Plain-GU-Boundaries.408 408 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -994.3 m 360.5 m
Po-Plain-GU-Boundaries.409 409 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -993.7 m 360.2 m
Po-Plain-GU-Boundaries.410 410 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -993.2 m 359.9 m
Po-Plain-GU-Boundaries.411 411 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -992.6 m 359.6 m
Po-Plain-GU-Boundaries.412 412 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -992.0 m 359.3 m
Po-Plain-GU-Boundaries.413 413 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -991.5 m 359.0 m
Po-Plain-GU-Boundaries.414 414 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -990.9 m 358.8 m
Po-Plain-GU-Boundaries.415 415 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -990.4 m 358.5 m
Po-Plain-GU-Boundaries.416 416 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -989.8 m 358.2 m
Po-Plain-GU-Boundaries.417 417 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -989.2 m 357.9 m
Po-Plain-GU-Boundaries.418 418 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -988.7 m 357.6 m
Po-Plain-GU-Boundaries.419 419 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -988.1 m 357.3 m
Po-Plain-GU-Boundaries.420 420 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -901.6 m 301.4 m
Po-Plain-GU-Boundaries.421 421 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -900.2 m 300.3 m
Po-Plain-GU-Boundaries.422 422 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -898.9 m 299.3 m
Po-Plain-GU-Boundaries.423 423 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -897.6 m 298.3 m
Po-Plain-GU-Boundaries.424 424 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -896.3 m 297.3 m
Po-Plain-GU-Boundaries.425 425 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -895.0 m 296.3 m
Po-Plain-GU-Boundaries.426 426 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -893.6 m 295.3 m
Po-Plain-GU-Boundaries.427 427 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -586.2 m 65.5 m
Po-Plain-GU-Boundaries.428 428 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -538.7 m 11.1 m
Po-Plain-GU-Boundaries.429 429 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -551.5 m 45.3 m
Po-Plain-GU-Boundaries.430 430 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -624.2 m 123.0 m
Po-Plain-GU-Boundaries.431 431 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -718.4 m 228.8 m
Po-Plain-GU-Boundaries.432 432 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -775.3 m 238.2 m
Po-Plain-GU-Boundaries.433 433 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -780.9 m 246.1 m
Po-Plain-GU-Boundaries.434 434 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -721.9 m 182.1 m
Po-Plain-GU-Boundaries.435 435 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -762.0 m 99.0 m
Po-Plain-GU-Boundaries.436 436 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1135.5 m 55.3 m
Po-Plain-GU-Boundaries.437 437 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1290.9 m 7.4 m
Po-Plain-GU-Boundaries.438 438 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1405.4 m 4.1 m
Po-Plain-GU-Boundaries.439 439 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1526.0 m 61.4 m
Po-Plain-GU-Boundaries.440 440 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1651.9 m 60.8 m
Po-Plain-GU-Boundaries.441 441 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1774.2 m 69.0 m
Po-Plain-GU-Boundaries.442 442 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1788.8 m 77.9 m
Po-Plain-GU-Boundaries.443 443 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1880.0 m 117.8 m
Po-Plain-GU-Boundaries.444 444 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1910.3 m 139.9 m
Po-Plain-GU-Boundaries.445 445 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1898.7 m 92.1 m
Po-Plain-GU-Boundaries.446 446 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1906.6 m 92.3 m
Po-Plain-GU-Boundaries.447 447 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1908.2 m 93.1 m
Po-Plain-GU-Boundaries.448 448 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1909.8 m 93.9 m
Po-Plain-GU-Boundaries.449 449 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1911.4 m 94.7 m
Po-Plain-GU-Boundaries.450 450 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1913.0 m 95.5 m
Po-Plain-GU-Boundaries.451 451 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1914.6 m 96.3 m
Po-Plain-GU-Boundaries.452 452 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1912.6 m 93.4 m
Po-Plain-GU-Boundaries.453 453 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -1914.1 m 94.2 m
Po-Plain-GU-Boundaries.454 454 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2024.4 m 137.6 m
Po-Plain-GU-Boundaries.455 455 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2079.1 m 106.7 m
Po-Plain-GU-Boundaries.456 456 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2125.4 m 249.3 m
Po-Plain-GU-Boundaries.457 457 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2186.7 m m
Po-Plain-GU-Boundaries.458 458 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2308.1 m m
Po-Plain-GU-Boundaries.459 459 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2269.7 m 409.2 m
Po-Plain-GU-Boundaries.460 460 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2314.0 m m
Po-Plain-GU-Boundaries.461 461 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2310.4 m m
Po-Plain-GU-Boundaries.462 462 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2311.6 m m
Po-Plain-GU-Boundaries.463 463 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2312.7 m m
Po-Plain-GU-Boundaries.464 464 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2313.8 m m
Po-Plain-GU-Boundaries.465 465 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2314.9 m m
Po-Plain-GU-Boundaries.466 466 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2316.1 m m
Po-Plain-GU-Boundaries.467 467 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2317.2 m m
Po-Plain-GU-Boundaries.468 468 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2318.3 m m
Po-Plain-GU-Boundaries.469 469 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2319.4 m m
Po-Plain-GU-Boundaries.470 470 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2320.6 m m
Po-Plain-GU-Boundaries.471 471 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2321.7 m m
Po-Plain-GU-Boundaries.472 472 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2388.6 m 331.6 m
Po-Plain-GU-Boundaries.473 473 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2353.2 m 293.1 m
Po-Plain-GU-Boundaries.474 474 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2410.1 m m
Po-Plain-GU-Boundaries.475 475 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2410.5 m m
Po-Plain-GU-Boundaries.476 476 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2432.3 m m
Po-Plain-GU-Boundaries.477 477 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2453.0 m m
Po-Plain-GU-Boundaries.478 478 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2460.4 m m
Po-Plain-GU-Boundaries.479 479 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2461.4 m m
Po-Plain-GU-Boundaries.480 480 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2462.6 m m
Po-Plain-GU-Boundaries.481 481 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2463.8 m m
Po-Plain-GU-Boundaries.482 482 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2465.0 m m
Po-Plain-GU-Boundaries.483 483 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2465.0 m m
Po-Plain-GU-Boundaries.484 484 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2466.4 m m
Po-Plain-GU-Boundaries.485 485 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2467.9 m m
Po-Plain-GU-Boundaries.486 486 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2468.4 m m
Po-Plain-GU-Boundaries.487 487 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2468.7 m m
Po-Plain-GU-Boundaries.488 488 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2469.2 m m
Po-Plain-GU-Boundaries.489 489 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2469.6 m m
Po-Plain-GU-Boundaries.490 490 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2470.1 m m
Po-Plain-GU-Boundaries.491 491 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2470.6 m m
Po-Plain-GU-Boundaries.492 492 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2471.0 m 407.2 m
Po-Plain-GU-Boundaries.493 493 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2471.5 m 407.6 m
Po-Plain-GU-Boundaries.494 494 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2472.0 m 408.1 m
Po-Plain-GU-Boundaries.495 495 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2472.4 m 408.5 m
Po-Plain-GU-Boundaries.496 496 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2472.9 m 408.9 m
Po-Plain-GU-Boundaries.497 497 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2473.3 m 409.4 m
Po-Plain-GU-Boundaries.498 498 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2473.8 m 409.8 m
Po-Plain-GU-Boundaries.499 499 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2562.4 m m
Po-Plain-GU-Boundaries.500 500 2 hlu5_PL hlu5_PL GE_3DModel The succession, lying on the post-Messinian unconfomity (PL unconformity in GeoMol Team, 2015 and D'Ambrogi et al., 2015), is represented by littoral-neritic to epi-bathyal deposits, locally including turbidites; it is constituted by clay, silty and sandy clay, alternating clay and quartz sand, with locally intercalated conglomerate and glauconitic sand. The age ranges from Zanclean to Gelasian. PlioceneSuccession lithostratigraphicUnit 1 PL_u unconformable_base 2 claystone part of siltstone part of sedimentaryProcess Zanclean Gelasian -2659.7 m m