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- W2355132008 abstract "The present-day tectonic framework of Turkey comprises mainly two strike-slip fault systems, namely dextral North Anatolian and sinistral East Anatolian faults. They are considered as the main cause of deformation patterns in Anatolia. These two mega shear systems meet at Kargapazarı village of Karlıova county. The area to the east of the junction has a transpressional tectonic regime between the Eurasian and Arabian plates and is characterized, based on field observation, by a network of faults defining a typical horsetail splay structure. The horsetail splay is interpreted as marking the termination of the North Anatolian Fault System (NAFS), which continues eastward into the Varto Fault Zone (VFZ) and then dies out. The present study reveals that the VFZ is made up of two main parts, namely the principal displacement zone (PDZ) and the transpressional splay zone (TPSZ), both characterized by the right-lateral strike-slip with reverse motion. However, the area to the east of Varto is characterized dominantly by reverse-thrust faults and E–W-trending faults as shown by focal mechanism solutions. The generation of the VFZ as a transpressional termination to the NAFS can be related directly to the block movements of the Eurasian, Anatolian, and Arabian plates." @default.
- W2355132008 created "2016-06-24" @default.
- W2355132008 creator A5017328289 @default.
- W2355132008 date "2016-05-12" @default.
- W2355132008 modified "2023-10-14" @default.
- W2355132008 title "The termination of the North Anatolian Fault System (NAFS) in Eastern Turkey" @default.
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- W2355132008 doi "https://doi.org/10.1080/00206814.2016.1175976" @default.
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