Supplementary Material 2 for Tosi et al.: Three-dimensional analysis of the Plio-Pleistocene sequence in the Venice Lagoon (Italy)

Figure 1S. a) Satellite image of the Venice coastland with the trace of the multi-channel seismic profiles and the location of the wells used in this study. b) Seismic-well tie along Line03. Note the deep fluvial erosion of the Messinian unconformity, the south-westward onlaps of PLC-2 and PLS-2 the prograding of PLS-4 toward the Venice lagoon. c) Seismic–well tie along Line04. In this section PLC-2 is represented by its distal (basinal) facies, while PLS-2 is absent due to its depositional limits. d) Seismic-well tie along Line05. Note PLC-2 downlaps on the Messinian unconformity and the  thinning of  PLS-3 toward South.