Possible role of fluid overpressure in the generation of earthquake swarms in active tectonic areas: The case of the Peloritani Mts. (Sicily, Italy)

The Peloritani Mts. (NE Sicily) are characterized by frequent seismicity. Between 1994 and 2006 more than
1000 earthquakes (1.0≤ML≤3.3) occurred, mostly as highly clustered swarms located at shallow depth near
the villages of Castroreale and Rodì Milici (western part of Peloritani Mts.). The same area is also characterized
by some geothermal springs and gas vents. Using a multidisciplinary approach, data were collected
on the tectonic setting, seismicity pattern and geochemical characteristics of fluid emissions, with the aim of
understanding the process of earthquake swarm generation beneath the investigated area.
Most of the gases emitted in the study area, in terms of focused and/or diffuse gas emissions often associated
with thermal fluids, is of mantle origin, as shown by their He isotopes ratio. On approaching the surface, deep
gases interact strongly with local aquifers. An estimate of both the surface efflux of mantle-derived gases
measured in focused emissions and of the P–T conditions of fluids in the local crust point to a pressurised gas
source that would be located at depth of 7–12 km, corresponding to the range of hypocentral depths of
seismic swarms. The complex network of tectonic structures in the area would act as high-permeability
pathways for the migration of sub-crustal fluids towards the surface. This scenario could be compatible with
a close interplay between pressurised mantle fluids at depth, nucleation of earthquakes due to higher-thanhydrostatic
pore pressure and release of mantle-derived gases at the surface. This sequence would be
repeated in time, thus producing the observed cycles in the local seismic activity.

Istituto Nazionale di Geofisica e Vulcanologia, sezione di Catania; Istituto Nazionale di Geofisica e
Vulcanologia, sezione di Palermo

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