GNGTS 2015 - Atti del 34° Convegno Nazionale

20 GNGTS 2015 S essione 1.1 Fig. 2 – Structural setting of the study area with isobaths contours of Pliocene units below the whole Po Plain (as reported by Consiglio Nazionale delle Ricerche, 1992) and main tectonic lineaments (after Fantoni and Franciosi, 2010) with the main events of the 2012 seismic sequence (modified after Malagnini et al., 2012). Some geological cross sections, well-known in literature, are also stressed: A) part of the section CC’ from Boccaletti et al. (2004); B) geological cross section built on the interpretation of the App_Or_1 seismic profile (modified from Carminati et al., 2010); C) geological cross section modified from Fantoni and Franciosi (2010). The general stratigraphy in the area of interest is summarized (box on the right-high corner), highlighting the presence of gas-bearing reservoir units (modified after Bertello et al., 2010). The sectionA crosses the area considered in this paper: on the bottom, a snapshot of the section A with a red rectangle that highlights the Sant’Alberto structure.