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  • 1
    Publication Date: 2013-10-09
    Description: On 2011 October 23, the Lake Van region in eastern Anatolia was hit by an M w  = 7.2 earthquake. The Van-Ercis earthquake (EQ) occurred 20 km east of Lake Van. Centroid moment tensors (CMT) for 108 events with M w between 4.0 and 7.2 are computed by applying a waveform inversion method on data from the Kandilli Observatory and Earthquake Research Institute (KOERI) broad-band seismic network. The time span of data covers the period between 2011 October 23 and 2012 February 24. The main shock is a shallow focus thrust event at a depth of 15 km. Focal depths of aftershocks range from 12 to 25 km. The seismic moment ( M 0 ) of the main shock is estimated to be 0.75 10 20 Nm. The focal mechanisms of the aftershocks are mainly thrust faulting with a variable and sometimes significant strike–slip component. This geometry indicates a thrust faulting regime with NE–SW trending direction of T -axis in the entire activated region. A stress tensor inversion of focal mechanism data is performed to obtain a more accurate picture of the Van-Ercis EQ stress field. The stress tensor inversion results show a predominant thrust stress regime with a NW–SE to NNE–SSW oriented maximum horizontal compressive stress ( S H ). The secondary fault system striking mostly ENE–WSW is activated generally with right-lateral strike–slip in the east of the main shock. This difference in mechanism suggest that towards the east, a different fault system is activated with respect to the NE–SW trending thrust faults beneath Van-Ercis region and more to the west. Thus, to first order, the Lake Van region is characterized by a homogeneous intraplate stress field.
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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  • 2
    Publication Date: 2007-02-01
    Description: We present an update of the local magnitude scale previously calibrated for northwestern Turkey by Baumbach et al. (2003). The path coverage in the westernmost part of the analyzed area has been increased, as well as the number of amplitudes for distance greater than 110 km. Furthermore, a set of recordings from accelerometric stations operated by the Kandilli Observatory and Earthquake Research Institute (KOERI) has been merged with the recordings by the Sapanca-Bolu and German Task Force seismological networks. In all, 4047 recordings from 528 earthquakes recorded by 31 seismometers and 23 accelerometers are considered to calibrate the local magnitude scale over a hypocentral distance range from 10 to 190 km. By analyzing the unit covariance matrix and the resolution matrix, we show how the source-to-station geometries of the seismic and strong-motion networks affect the uncertainties of the computed station corrections, attenuation coefficients, and magnitudes. The assumptions made concerning the reference station correction, and the change in the amplification for the Wood-Anderson torsion seismograph from 2800 to 2080 (Uhrhammer and Collins, 1990) introduced an offset of about 0.34 in the magnitudes with respect to Baumbach et al. (2003), with the updated local magnitude scale ranges from 0.50 to 5.91. The distribution of the residuals with distance confirms that the extension of both the magnitude and distance ranges and the improved path coverage have preserved the high quality that characterized the data set analyzed by Baumbach et al. (2003).
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
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