Uplift of the Emei Shan, western Sichuan Basin: Implication for eastward propagation of the Tibetan Plateau in Early Miocene
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- 作者：Kai Menga ; Michael.meng@mail.iggcas.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Erchie Wanga ; b ; Gang Wangc
- 关键词：Emei Shan ; Mountain uplift ; Apatite fission track ; Eastern margin of the Tibetan Plateau
- 刊名：Journal of Asian Earth Sciences
- 出版年：2016
- 出版时间：1 January 2016
- 年：2016
- 卷：115
- 期：Complete
- 页码：29-39
- 全文大小：6802 K
文摘
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Uplift of the Emei Shan occurred ca. 25–20 Ma.
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Uplift of the Emei Shan indicated the time-transgressive propagation of the EMTP.
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The Yaan−Emei Shan fold belt absorbed most of regional deformation.
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The Emei Shan region was intended into the Sichuan Basin bounded by two strike-slip faults.