GNGTS 2013 - Atti del 32° Convegno Nazionale

Tab. 1 – Interpreted seismic sections and related calibration wells used for the depth conversion processes. The seismic lines, wells location and interpreted sections are shown in Fig. 2. Seismic Section Section Length (km) Calibration Well AA’ 28 Vicenza 1 = Vi1 AA-AA’ 36.5 Ballan 1 = Ba1 BB’ 27.8 S. Angelo Piove di Sacco 1 = Sa1 Legnaro 1 = Le1 CC-CC’ 30.9 Villadose 1 = Vd1 Codevigo 1 = Co1 CC’ 28 - DD’ 24 Corte Vittoria 1 = Cv1 EE’ 24 Pomposa 1 = Po1 Fig. 2 – Cross-sections sub– orthogonal to the SVFS ob- tained through the seismic sections interpretation and the subsequent depth conversion process. Different stratigraph- ic horizons were recognised leading to a subdivision be- tween the southern sections, located close the Po delta, and the northern ones, located close to the relief. Fault traces associated to the Schio-Vicen- za fault system are recognised (SV: Schio–Vicenza fault; CP: Conselve–Pomposa fault; TV: Travettore–Codevigo fault). Mesozoic extensional faults (M) and an Apennine reverse fault (A) are also depicted. The faults divide the subsurface in a mosaic of blocks deepen- ing towards NE. The map ev- idences also the border of the basins and swells representing the Mesozoic architecture of the study area (T: Trento plat- form-plateau, B: Belluno ba- sin, NA: Northern Adriatic ba- sin, F: Friuli platform-plateau; see also Fig. 1). 188 GNGTS 2013 S essione 1.2