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Swiss Journal of Geosciences
Fig. 10 | Swiss Journal of Geosciences

Fig. 10

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

Fig. 10

Conceptual model illustrating a possible stratigraphic and tectonic evolution of the Epiligurian wedge-top basin from Rupelian to Serravallian as derived from present study and from literature (Papani et al. 1987, 2002; De Nardo et al. 1991; Cerrina Feroni et al. 2002a, b). The scales indicate order of magnitude and vertical scale is exaggerated. Note the change of scale between stages 1 (focusing on the study area of Fig. 4) and stages 2–6 (focusing on the Epiligurian wedge-top basin preserved in the Vetto-Carpineti syncline in Fig. 2); in stages 2–6, the area analyzed in this study is marked by the rectangle

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