A temporary seismic monitoring of the Sulmona area (Abruzzo, Italy) for seismotectonic purposes

The seismogenic potential of active faults in the Abruzzo region of central Italy has been tragically brought to the general attention by the April 6, 2009 L'Aquila earthquake. In this region, a system of SW-dipping normal faults has been active both in historical and recent times, with at least three moderate-to-large earthquakes (Avezzano 1915, Barrea 1984, and L'Aquila 2009) and several minor seismic sequences. Some highly populated areas, like the Sulmona basin at the hanging wall of the Mt. Morrone fault (a segment capable of releasing destructive earthquakes, Mmax~6.7), have not experienced significant earthquakes in the last millennium; the time lapse since the last event should therefore be comparable with the recurrence time assigned to this fault, enhancing its contribution to seismic hazard in a time-dependent perspective. With the aim of increasing our knowledge on the active deformation pattern, geometry and seismogenic depth of the potential structures by means of low-mag...