U-Pb zircon ages, field geology and geochemistry of the Kermanshah ophiolite (Iran): From continental rifting at 79 Ma to oceanic core complex at ca. 36 Ma in the southern Neo-Tethys
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- 作者：Songjian Aoa ; asj@mail.igcas.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Wenjiao Xiaoa ; b ; Morteza Khalatbari Jafaric ; Morteza Talebianc ; Ling Chena ; Bo Wana ; b ; Weiqiang Jia ; Zhiyong Zhanga
- 关键词：Oceanic core complex ; Kermanshah ophiolite ; Neo-Tethys ; U&ndash ; Pb age ; Iran
- 刊名：Gondwana Research
- 出版年：2016
- 出版时间：March 2016
- 年：2016
- 卷：31
- 期：Complete
- 页码：305-318
- 全文大小：4332 K
文摘
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The older part of Kermanshah ophiolite was generated by detachment faulting at 79 Ma.
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The younger part of ophiolite originated was from the oceanic core complex at 36 Ma.
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The Zagros ophiolite belt is part of an accretionary prism.
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Neo-Tethys Ocean may have closed after 36 Ma.