Geochronology and petrogenesis of granitoids and associated mafic enclaves from Xiate in Chinese Southwest Tianshan: Implications for early Paleozoic tectonic evolution
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- 作者：Long-Long Goua ; b ; LLgou@nwu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Li-Fei Zhangb
- 关键词：Granitoids ; Continent marginal arc ; Southwest Tianshan ; Magma mixing ; Central Asian Orogenic Belt
- 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：40-61
- 全文大小：5960 K
文摘
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The Dongdeguli granitoids and Changawuzi mylonitic pluton formed at ca. 443–453 Ma.
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The Dongdeguli granitoids and their mafic enclaves were formed by magma mixing.
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The Late-Ordovician northward subduction of paleo-South Tianshan oceanic crust.