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Swiss Journal of Geosciences
Fig. 6 | Swiss Journal of Geosciences

Fig. 6

From: The Epiligurian wedge-top succession in the Enza Valley (Northern Apennines): evidence of a syn-depositional transpressive system

Fig. 6

a The outcrop of the arenaceous-conglomeratic lithofacies of Ranzano Formation (Ran2a) located on the hydrographic right bank of Enza River, between Ranzano and Taviano villages. The dashed lines mark the bases of the beds that show lenticular geometries. Approximately along the Enza riverbed, the main erosional unconformity at the base of Ran 2a lithofacies (see Sect. 4.1) is well exposed in tiny outcrops (e.g. b) where the on-lap relationship between Ran 2a lithofacies (Rupelian) and the Ligurian Flysch (uppermost Cretaceous) is clearly shown

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