The temporal evolution of the active margin along the Southeast Anatolian Orogenic Belt (SE Turkey): Evidence from U-Pb, Ar-Ar and fission track chronology
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- 作者：Fatih Karaoğlana ; fkaraoglan@cu.edu.tr" class="auth_mail" title="E-mail the corresponding author ; Osman Parlaka ; Ewald Hejlb ; Franz Neubauerb ; Urs Klö ; tzlic
- 关键词：Southeast Anatolia ; Granitoids ; Apatite Fission Track ; Ar&ndash ; Ar ; LA-ICP-MC-MS zircon U&ndash ; Pb ; Convergent Margin
- 刊名：Gondwana Research
- 出版年：2016
- 出版时间：May 2016
- 年：2016
- 卷：33
- 期：Complete
- 页码：190-208
- 全文大小：6013 K
文摘
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The first continental collision occurred between Bitlis–Pütürge and Tauride platforms.
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Granitoids continued uplifting during early–middle Eocene in an extensional setting.
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The final collision between Tauride and Arabian platforms occurred in Oligocene.