Abstract
In the early morning hours on Wednesday November 08, 2006 at 04:32: 10(GMT) a small earthquake of M-L 4.1 has occurred at southeast Beni-Suef, approximately 160 km SEE of Cairo, northern Egypt. The quake has been felt as far as Cairo and its surroundings while no casualties were reported. The instrumental epicentre is located at 28.57 degrees N and 31.55 degrees E. Seismic moment is 1.76 E14 Nm, corresponding to a moment magnitude M-w 3.5. Following a Brune model, the source radius is 0.3 km with an average dislocation of 1.8 cm and a 2.4 MPa stress drop. The source mechanism from a first motion fault plane solution shows a left-lateral strike-slip mechanism with a minor dip-slip component along fault NNW striking at 161 degrees, dipping 52 degrees to the west and rake -5 degrees. Trend and plunging of the maximum and minimum principle axes P/T are 125 degrees, 28 degrees, 21 degrees, and 23 degrees, respectively. A comparison with the mechanism of the October, 1999 event shows similarities in faulting type and orientation of nodal planes.
Eight small earthquakes (3.0 <= M-L < 5.0) were also recorded by the Egyptian National Seismological Network (ENSN) from the same region. We estimate the source parameters and fault mechanism solutions (FMS) for these earthquakes using displacement spectra and P-wave polarities, respectively. The obtained source parameters including seismic moments of 4.9 x 10(12)-5.04 x 10(15) Nm, stress drops of 0.2-4.9 MPa and relative displacement of 0.1-9.1 cm. The azimuths of T-axes determined from FMS are oriented in NNE-SSW direction. This direction is consistent with the present-day stress field in Egypt and the last phase of stress field changes in the Late Pleistocene, as well as with recent GPS measurements. (c) 2008 Elsevier Ltd. All rights reserved.