An overview of the crustal structure of the Tibetan plateau after 35 years of deep seismic soundings

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• 作者：Zhongjie Zhang^a ; ^{zhangzj@mail.iggcas.ac.cn} ; Yangfan Deng^b ; ^c ; Jiwen Teng^a ; Chunyong Wang^d ; Rui Gao^e ; Yun Chen^a ; Weiming Fan^b
• 关键词：Wide-angle seismic profiling ; Crustal thickness ; Tibetan plateau
• 刊名：Journal of Asian Earth Sciences
• 出版年：2011
• 出版时间：3 March 2011
• 年：2011
• 卷：40
• 期：4
• 页码：977-989
• 全文大小：3293 K

文摘

Since the pioneer wide-angle seismic profile along the Yadong–Gulu rift acquired in 1974 by the ex-Institute of Geophysics, Chinese Academy of Sciences (CAS), several research programs aimed to deep geophysics, performed thanks to the participation of Chinese national and international institutions, have been developed during last 35 years, including 23 wide-angle seismic profiles with total length of about 6000 km. These profiles are unevenly distributed, most of them in eastern Tibet and few profiles in western Tibet. In this paper, we make a summarized presentation of all these wide-angle seismic profiles and provide an overall view of the seismic velocity structure of the crust beneath the broad Tibetan plateau, which is the product of the continuous convergence and collision of the Indian and Eurasian plates since about 50 Ma ago. Different patterns of crustal thickness variation related to the tectonic blocks and along suture zones of the region are displayed. The crust thickness is confirmed to be about 70–75 km under southern Tibet, and 60–65 km under northern, northeastern and southeastern Tibet. The leading edge of the subducted lithosphere reaches the northern margin of the plateau and directly contacts with Tarim Basin. Westward of the 90°E boundary, the Indian crust is moving towards the northern edge of the plateau and collides with Tarim Basin at 80°E while reach the Bangong–Nujiang suture belt at 88°E; eastward of the 90°E boundary, the northern edge of the crust should be at 50–100 km south of Bangong–Nujiang suture. The results supply helpful constrains to understand the mechanism of the continent–continent collision and its consequences in the plateau and neighbouring areas.