Central and eastern Anatolian crustal deformation rate and velocity fields derived from GPS and earthquake data
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- 作者：N.M. Simã ; oa ; nmmsimao@gmail.com" class="auth_mail" title="E-mail the corresponding author ; S.S. Nalbanta ; F. Sunbula ; A. Komec Mutlub
- 关键词：East Anatolian Fault ; North Anatolian Fault ; seismic hazard ; strain-rate ; Arabian&ndash ; Anatolian convergence ; seismotectonics of Anatolia
- 刊名：Earth and Planetary Science Letters
- 出版年：2016
- 出版时间：1 January 2016
- 年：2016
- 卷：433
- 期：Complete
- 页码：89-98
- 全文大小：2368 K
文摘
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New Anatolian strain-rate & kinematic model for central & eastern & central region.
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Surface deformation observed similar to that of lithospheric mantle.
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Regions that deform most are situated above strong gradients in crustal thickness.
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Central Anatolia is more rapidly moving towards the west than eastern Anatolia.
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Movement rate differences leads to observed extension deformation in Iskenderun Bay.