Fig. 5From: The succession of the Val Marecchia Nappe (Northern Apennines, Italy) in the light of new field and biostratigraphic dataMonte Morello Fm.: alternation of calcareous and marly turbidites (a) and detail of the carbonate turbidite succession (b) in the Tiber valley north of Pieve Santo Stefano; siliciclastic arenites interbedded with carbonate turbidites (c) and ophiolite-derived debrite (d) along the Pieve Santo Stefano-Viamaggio road. Hammer is 25 cm longBack to article page