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CAO Xiao lin, HONG Xue hai, CAO Jun xing (Chengdu University of Technology, China)  
The amplitude at about 20 s period and 40 s period of surface waveform through Qinghai Tibet Plateau is lower than both sides. This implies there exists one or two lower velocity layers in the Qinghai Tibet Plateau crust. The authors invert surface waveform for crust upper mantle by simulated annealing, which can solve the non linear global optimizing problem. The results show the region of Tibet plateau exists low velocity layers at about 20 km depth in crust. Under the Himalayan Mountain, there exist a low velocity layer at about about 60 km depth. Low velocity layer in the crust is one of the most important dynamic boundary conditions during the uplift of Qinghai Tibet Plateau.
【Fund】: 国家自然科学基金重点资助项目! (49734150 );; 国家高性能计算基金
【CateGory Index】: P313
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