Comment on “The Fethiye-Burdur Fault Zone: A component of upper plate extension of the subduction transform edge propagator fault linking Hellenic and Cyprus Arcs, Eastern Mediterranean. Tectonophysics 635, 80-99” by J. Hall, A.E. Aksu, İ. Elitez, C. Yaltırak, G. Çiftçi
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- 作者：M. Cihat Alç ; iç ; ek ; alcicek@pau.edu.tr" class="auth_mail" title="E-mail the corresponding author
- 关键词：Extensional tectonics ; Neogene ; Terrestrial basin ; SW Anatolia ; Eastern Mediterranean
- 刊名：Tectonophysics
- 出版年：2015
- 出版时间：28 November 2015
- 年：2015
- 卷：664
- 期：Complete
- 页码：1-4
- 全文大小：765 K
文摘
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NE-trending Pliny–Strabo trench has envisaged being continued into Anatolia as strike-slip fault.
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It is unproven by field map, kinematics, fault plane solutions of earthquakes and subsurface data.
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SW Anatolia occupies an array of NE-trending extensional basins bounded by dip-slip faults.