Tectono-stratigraphic evolution of the Southern Campania Margin: a key area for the evolution of the Tyrrhenian-Apennine system | Oil & Gas Science and Technology

Dynamics of sedimentary basins and underlying lithosphere at plate boundaries: The Eastern Mediterranean

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Fig. 7.

(a) Isopach map of the Unit A and geological sections (a1 and a2) through the Salerno Bay Basin (SBB) and Cilento Basin (CB). Faults are Lower Pleistocene in age. Contour interval is 150 m. (b) Isopach map of the Unit B and geological sections (b1 and b2) through the Salerno Valley-Capri Basin (SV-CB) and Salerno-Cilento Basin (SCB). BFF = Banco di Fuori Fault, SPF = Sorrento Peninsula Fault. Faults are early Middle Pleistocene in age. Contour interval is 70 m. (c) Isopach map of the Unit C and geological section (c1) through the Sapri Basin (SB). SBF = Sapri Basin Fault. Faults are Late Middle Pleistocene-Present in age. Contour interval is 100 m. Maps coordinate system: UTM, WGS84.

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