JOURNAL OF ASIAN EARTH SCIENCES, cilt.92, ss.168-186, 2014 (SCI-Expanded)
An intraplate earthquake of magnitude Mw 7.2 occurred on a NE-SW trending blind oblique thrust fault in accretionary orogen, the Van region of Eastern Anatolia on October 23, 2011. The aftershock seismicity in the Van earthquake was not continuous but, rather, highly discrete. This shed light on the chaotic non-uniformity of the event distribution and played key roles in determining the seismic coupling between the rupturing process and seismogeneity.