Quaternary normal faulting in southeastern Sicily (Italy): A seismic source for the 1693 large earthquake

We present geological and morphological data, combined with an analysis of seismic reflection lines across the Ionian offshore zone and information on historical earthquakes, in order to yield new constraints on active faulti ng in southeastern Sicily. This region, one of the most seismically active of the Mediterranean, is affected by WNW-ESE regional extension producing n ormal faulting of the southern edge of the Siculo-Calabrian rift zone. Our data describe two systems of Quaternary normal faults, characterized by dif ferent ages and related to distinct tectonic processes. The older NW-SE-tre nding normal fault segments developed up to approximate to 400 kyr ago and, striking perpendicular to the main front of the Maghrebian thrust belt, bo und the small basins occurring along the eastern coast of the Hyblean Plate au. The younger fault system is represented by prominent NNW-SSE-trending n ormal fault segments and extends along the Ionian offshore zone following t he NE-SW-trending Avola and Rosolini-Ispica normal faults. These faults are characterized by vertical slip rates of 0.7-3.3 mm yr(-1) and might be ass ociated with the large seismic events of January 1693. We suggest that the main shock of the January 1693 earthquakes (M similar to 7) could be relate d to a 45 km long normal fault with a right-lateral component of motion. A long-term net slip rate of about 3.7 mm yr(-1) is calculated, and a recurre nce interval of about 550 +/- 50 yr is proposed for large events similar to that of January 1693.