Fig. 1From: The Epiligurian wedge-top succession in the Enza Valley (Northern Apennines): evidence of a syn-depositional transpressive system a Schematic geological map of the Northern Apennines and location of the Vetto-Carpineti syncline (Fig. 2). Modified after Bernini, Vescovi, Artoni (unpublished), already modified from Bernini et al. (1997), Boccaletti and Coli (1982) and Bigi and Scandone (1991). b Geological map of the Emilian Apennines between the Parma Valley and Monte Prado with the location of the studied area (Fig. 4). Modified after Vescovi (2005)Back to article page