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Publications by [Çolak S.]

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THE PALU-ULUOVA STRIKE-SLIP BASIN IN THE EAST ANATOLIAN FAULT SYSTEM, TURKEY: ITS TRANSITION FROM THE PALAEOTECTONIC TO NEOTECTONIC STAGE (2011)
<p>The East Anatolian fault system (EAFS) is the 80-km-wide, 700-km-long, NE trending sinistral strike-slip fault system forming a seismically very active intracontinental transfom fault boundary. It is located between Karlıova County in the northeast and ...
Reference: Turkish Journal of Earth Sciences (Turkish J. Earth Sci.), Vol. 21, 2012, pp. 1–. Copyright ©TÜBİTAK First published online 16 August 2011