Foreshock sequence of September 26th, 1997 Umbria-Marche earthquakes

On September 3(rd) (22:07 UTC), 1997 a small earthquake with Mw=4.54 started the foreshocks sequence (approximate to 1500 events with M-L <3.1) of the September 26(th) seismic sequence. Two days after, three seismic stations of the University of Camerino were installed around the macroseismic epicenter of the foreshock. We present in this paper the location of foreshocks (with 2.1 <M-L<3.3) which occurred between September 3(r)d and 26(t)h. Foreshocks location, with horizontal (ERH) and vertical (ERZ) error less than 1.5 km, define an area approximate to4 km large. Foreshocks have been localized between the epicenters of the two major events of September 26(t)h, which occurred at 00:33 UTC with Mw=5.6 and at 09:40 UTC with Mw=6.0 (Amato et al., 1998; Ekstrom et al., 1998). In a vertical cross-section, hypocenters show a low angle (approximate to 30 degrees) structure with SW dip-direction. Focal mechanisms for three of the major events show dip-slip fault solutions with strike direction of about N130, in agreement with the CMT solutions of September 3(r)d and September 26(t)h earthquakes (Ekstrom et al., 1998). Data recorded at two stations Popola (POP) e Capodacqua (CPQ) located on the rupture area of the September 26(t)h faults, allowed us to calculate a mean Vp/Vs ratio of 1.84 +/-0.03 for the foreshock. This value is lower than the Vp/Vs ratio of 1.89 +/-0.02 calculated for the aftershock sequence occurred in the same area. Besides, the Vp/Vs ratio during the foreshocks sequence is not stable in time but it seems to increase approaching September 26(t)h. After September 26(t)h mainshocks, this value tends to stabilize around a higher value of 1.89. Following the dilatancy model, we suggest that the relative low Vp/Vs ratio before the main shocks could indicate the presence of fluid in the focal volume. The presence of fluids could have increased the effective stress on the fault plane and could be responsible for the long foreshock activity before the two main earthquakes of September 26(t)h. Therefore, we suggest that this foreshock activity could have also contributed to reduce the friction along the September 26(t)h fault plane, breaking the active structure in two smaller segments. In this hypothesis, foreshock activity could have drastically contributed to mitigate the seismic potential of the Colfiorito's active structure.