GNGTS 2017 - 36° Convegno Nazionale

GNGTS 2017 S essione 1.2 109 Fig. 1 - A) The Aeolian-Tindari-Letojanni Fault System (ATLFS) is a regional deformation belt extending from the central sector of theAeolianArchipelago to the eastern coast of Sicily and separating two active tectonic compartments: a contractional one to the west and an extensional one to the north-east. In its north-western portion, the ATLFS system connects with the eastern branches of the Sisifo-Aliἀcudi transpressional fault belt (SAFS). The yellow stars represent the location of the Mw=6.2, 1786 and Mw=6.1, 1978 earthquakes. B) Multidisciplinary dataset considered in this study. Data conἀsist of field-based structural analyses carried out along the Lipari-Vulcano complex and the Peloritani Mts. (80 sites of measurements), high- and very-high resolution seismic profiles (~500 km) and swath bathymetry data (1000 km²) acquired in the Gulf of Patti, seismological (from 1999 to 2015) and geodetic (from 1996 to 2008) measurements.