Abstract: The Crustal-scale Shortening on the Eastern Margin of the Tibet Plateau: the Main Mechanism of Uplift--Revealed from Deep Seismic Reflection Profiles Across the Min Shan and Hu Ya Faults (AGU Fall Meeting 2018)

The Crustal-scale Shortening on the Eastern Margin of the Tibet Plateau: the Main Mechanism of Uplift--Revealed from Deep Seismic Reflection Profiles Across the Min Shan and Hu Ya Faults

Rui Gao^1,2, Xiao Xu¹, Xiaoyu Guo¹, Wenhui LI³, Hongqiang Li⁴, Haiyan Wang², Xingfu Huang⁵, Zhanwu Lu² and Zhuo Ye⁶, (1)Sun Yat-Sen University, School of Earth Sciences and Engineering, Guangzhou, China, (2)Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China, (3)State Key Laboratory of Deep Earth and Mineral Exploration, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China, (4)Chinese Academy of Geological Sciences, SinoProbe Center, Beijing, China, (5)School of Earth Sciences and Engineering, Sun Yat-Sen University, Guangzhou, China, (6)Chinese Academy of Geological Sciences, Beijing, China

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