GNGTS 2016 - Atti del 35° Convegno Nazionale

GNGTS 2016 S essione 1.2 211 Geophysical investigations of the crustal structure of the Hyblean Plateau include several velocity tomography studies, in which different techniques and datasets were considered (e.g. Di Stefano et al. , 1999; Barberi et al. , 2004; Scarfì et al. , 2007; Brancato et al. , 2009; Musumeci et al. , 2014). Fig. 1 – P-waves velocity model resulting from the 3D inversion. S-N and W-E vertical sections along the traces reported at 0 km level are also shown. On the 0 km layer the main structural features are reported with grey lines. The zones with RDE ≥ 0.4 SF ≤ 3.5; DWS ≥ 100 are shown with thick black, dotted white and dashed white contour lines, respectively.