Origin and evolution of the Tengchong block, southeastern margin of the Tibetan Plateau: Zircon U-Pb and Lu-Hf isotopic evidence from the (meta-) sedimentary rocks and intrusions
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- 作者：Dapeng Lia ; b ; Yuelong Chena ; chyl@cugb.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Kejun Houc ; Zhaohua Luoa
- 关键词：Detrital zircon ; U&ndash ; Pb ages ; Hf isotopes ; The Tibetan plateau ; Eastern Gondwana
- 刊名：Tectonophysics
- 出版年：2016
- 出版时间：26 September 2016
- 年：2016
- 卷：687
- 期：Complete
- 页码：245-256
- 全文大小：3992 K
文摘
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The paragneisses in Gaogigongshan Grp. deposited in the Late Paleozoic.
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The Tengchong block originated from Indian margin.
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The crust activated after Paleozoic.