GNGTS 2015 - Atti del 34° Convegno Nazionale

Fig. 3 – a: On the top, P velocity model for the section E-F superimposed by P ray density. In the bottom, it is shown the corresponding interpretation of geological section Dogna-Forni di Sopra with the simplified stratigraphic column (Ponton, 2010 modified). b: P velocity model for the section Bate (Slovenia)-Zell (Austria) superimposed by P-ray density. With the black arrow, is indicated the Idrija fault. GNGTS 2015 S essione 1.2 73