RECENT SEISMICITY (2000-2007) IN THE TIBURTINI-PRENESTINI MOUNTAINS REGION (LATIUM, ITALY)

摘要

A detailed knowledge of the seismicity distribution enables us to gain a better understanding of the recent tectonic evolution andthe present-day state of stress of the Tiburtini and Prenestini Mountains region, whose seismic importance is related with thenearness to the town of Rome. It has been carried out an analysis of the seismicity of the region using the data recorded by thepermanent stations belonging to the Italian National Seismic Network (RSNC) from 2000, and subsequently integrated with dataof local seismic network from 2003 to 2007. The increase of the number of stations in the last years allow us to obtain betterquality earthquake localization as before done. We have produced a large database of re-picked events collecting arrival times ofP and S waves of local earthquakes with magnitude larger than 2.0, belonging to the 2000-2007 period.The work is subdivided into three step. The first one consists in the determination of the VP/VS ratio using the modified Wadatimethod. In the second step we perform the analysis of the 1D velocity model that better approximates the structure of the crustin the studied area using the VELEST code (Kissling et al., 1995). Finally, we have the step with earthquake locations and focalmechanisms computation using the first motion polarities method. Fault plane solutions are selected following the two qualityfactors defined by the FPFIT code (Reasenberg and Oppenheimer, 1985). For the determination of the regional stress field it isused the focal mechanism inversion method elaborated by Gephart and Forsyth (1984). These results are compared with thoseavailable from the historical seismicity that struck the region under study.