“…and [e.g., King, 1985;Baubron et al, 2002;Ciotoli et al, 2007;Fu et al, 2008;Walia et al, S 2009;Ciotoli et al, 2014;Bigi et al, 2014;Sciarra et al, 2014]. Furthermore, over the past several years' soil gases has captured considerable attention as earthquake precursors [Wakita et al, 1980;Reddy et al, 2004;Walia et al, 2009;Perez et al, 2007;Ghosh et al, 2009;Hashemi et al, 2013;Petraki et al, 2015], in fact that the stress/strain changes related to seismic activity may force crustal fluid to migrate up, especially along active faults, thereby altering the geochemical characteristics of the fault zone at surface [Rice, 1992;Sibson, 2000;Collettini et al, 2008]. The migration of these gases by diffusion and/or advection along buried active faults can generate shallow anomalies with concentrations significantly higher than background levels; these anomalies can provide reliable information about the location and the geometry of the shallow fracturing zone, as well as about the permeability within the fault zone [King et al, 1996;Baubron et al, 2002;Ciotoli et al, 2007;Annunziatellis et al, 2008;Bigi et al, 2014;Sciarra et al, 2014].…”