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Source mechanism of the 23 October, 2011, Van (Turkey) earthquake (Mw = 7 1) and aftershocks with its tectonic implications

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Figure

Fig. 1.(a) The general neotectonic map of Anatolia. K—Karl ova, KM—Kahramanmaras¸, DSFZ—Dead Sea Fault Zone, EAFZ—East Anato-lian Fault Zone, NAFZ—North Anatolian Fault Zone (S¸eng¨or et al., 1985; Barka, 1992; Bozkurt, 2001)
Table 1. Historical and Instrumental period earthquakes (Ergin et al., 1967; Alsan et al., 1975; Soysal et al., 1981; Ambraseys, 1988; Eyidogan et al.,1991; Turkelli et al., 2003).
Fig. 2.The fault plane solutions of the main shock and 21 aftershocks of the Van earthquake with the surface ruptures which occurred duringthe earthquake, A: Alak¨oy, B: Bardakc¸ı, Ko: Kolsatan, K: Kozluca, Y: Yalnıza˘gac¸, S: Satıbey, As: As¸ıt, Gu: G¨uls
Fig. 3. (a) A view of left-lateral offset on a concrete block, caused by the MSR. (b) A view from the main surface rupture (MSR) on the Topaktas¸ road.The vertical thrust offset is approximately 0.1 m
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