Neogene-Quaternary evolution of the Tefenni basin on the Fethiye-Burdur fault zone, SW Anatolia-Turkey
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- 作者：Rahmi Aksoy ; raksoy@selcuk.edu.tr" class="auth_mail" title="E-mail the corresponding author ; Sü ; leyman Aksarı suleymanaksari@gmail.com" class="auth_mail" title="E-mail the corresponding author
- 关键词：Fethiye-Burdur fault zone ; Tefenni basin ; Neogene-Quaternary ; Kinematic analysis ; Western Anatolia
- 刊名：Journal of African Earth Sciences
- 出版年：2016
- 出版时间：June 2016
- 年：2016
- 卷：118
- 期：Complete
- 页码：137-148
- 全文大小：5539 K
文摘
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Tefenni basin contains infill of middle-upper Miocene-Quaternary sediments.
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NE-SW trending sinistral oblique-slip and normal faults main structure of the basin.
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Results of fault-slip data analysis are presented from the Tefenni basin.
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Two different deformation regimes governed the basin since upper Miocene.
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Tefenni basin is a transtensional basin.