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Over the last decade electromagnetic (EM) measurements have provided new constraints on the upper-crustal&#13; structure of the major fault zones in the world, both when they act as conduit and as a barrier, due to strong sensitivity&#13; of resistivity to fluids circulation and mineralization. On the track of a high impact magnetotelluric (MT)&#13; study performed across the San Andreas Fault, high resolution EM data were collected in the Colfiorito epicentral&#13; area along profiles crossing some main fault lineaments. Being the study focussed both on shallow that on intermediate&#13; resistivity distribution in the brittle upper-crust, a MT profile was integrated by several electrical resistivity&#13; tomographies (ERT). The latter were successful in locating faults even where the structures are buried by a wide&#13; covering of Quaternary deposits and in the recognition of different electrical signatures of the faults. MT resistivity&#13; model crossing Mt. Prefoglio normal fault clearly imaged the typical thrust structures of the area and a high&#13; conductive zone spatially related to the fault. Seismicity seems to be located outside such conductive area, whose&#13; behaviour suggests a fluidised and altered zone incapable of supporting significant stress internally

Shallow to intermediate resistivity features of the Colfiorito Fault System inferred by DC and MT survey