Late Devonian-Early Carboniferous magmatism in the Lhasa terrane and its tectonic implications: Evidences from detrital zircons in the Nyingchi Complex
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- 作者：Liang Guoa ; lguo@cug.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Hong-Fei Zhanga ; Nigel Harrisb ; Wang-Chun Xua ; Fa-Bin Panc
- 关键词：Lhasa terrane ; Detrital zircon ; Zircon trace-element ; Back-arc basin ; Tectonic evolution
- 刊名：Lithos
- 出版年：2016
- 出版时间：15 February 2016
- 年：2016
- 卷：245
- 期：Complete
- 页码：47-59
- 全文大小：3038 K
文摘
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The metasedimentary rocks in Nyingchi Complex contain abundant 330–364 Ma detrital zircons.
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The 330–364 Ma detrital zircons were derived from the Lhasa terrane.
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The Late Devonian-Early Carboniferous magmatism in the Lhasa terrane.
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Late Devonian-Carboniferous magmatic rocks in the Lhasa terrane formed in an arc-back-arc setting.