Crustal anisotropy and deformation of the southeastern margin of the Tibetan Plateau revealed by Pms splitting
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- 作者：Yan Caia ; Jianping Wua ; b ; wjpwu@cea-igp.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Lihua Fanga ; b ; Weilai Wanga ; Shuang Yic
- 关键词：Tibetan Plateau ; Anisotropy ; Receiver function ; Crustal deformation ; Pms splitting
- 刊名：Journal of Asian Earth Sciences
- 出版年：2016
- 出版时间：1 May 2016
- 年：2016
- 卷：121
- 期：Complete
- 页码：120-126
- 全文大小：2881 K
文摘
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The crustal anisotropy is primarily generated within the middle and lower crust.
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The differential movement may cause the anisotropy in the middle and lower crust.
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The crustal deformation near the faults mainly result from the strike-slip motion.