Crustal and Uppermost Mantle Heterogeneities Across the Ailaoshan Red River Shear Zone, SE Tibet: Implications for Cenozoic Magmatic Activity

The Ailaoshan Red River shear zone (ARSZ) was formed in the Mesozoic as a suture zone between the Indochina block and the Yangtze craton. Since the Cenozoic, block extrusion due to the Indo-Asian collision has reactivated the fault zone and caused large-scale shearing. Affected by the Cenozoic oroge...

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Main Authors: Xu, Mijian, Yu, Dayong, Huang, Zhouchuan, Tong, Ping, Hao, Shijie, Ruan, Youyi, Han, Cunrui
其他作者: School of Physical and Mathematical Sciences
格式: Article
語言:English
出版: 2023
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在線閱讀:https://hdl.handle.net/10356/170960
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