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Volume 20 Issue 2
Apr 2009
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Article Contents
Xiaosong Xiong, Rui Gao, Qiusheng Li, Zhanwu Lu. Moho Depth of Qinghai-Tibet Plateau Revealed by Seismic Probing. Journal of Earth Science, 2009, 20(2): 448-463. doi: 10.1007/s12583-009-0037-9
Citation: Xiaosong Xiong, Rui Gao, Qiusheng Li, Zhanwu Lu. Moho Depth of Qinghai-Tibet Plateau Revealed by Seismic Probing. Journal of Earth Science, 2009, 20(2): 448-463. doi: 10.1007/s12583-009-0037-9

Moho Depth of Qinghai-Tibet Plateau Revealed by Seismic Probing

doi: 10.1007/s12583-009-0037-9
Funds:

the National Natural Science Foundation of China 40830316

the National Natural Science Foundation of China 40874045

International Sciences and Technology Cooperation 2006DFA21340

the Special Fund for Sciences and Technology Research of Public Welfare Trades 200811021

the Key Innovation Project for Sciences and Technology of the Ministry of Land and Resources Trades 1212010711813

the China Geological Survey and Resources Land Investigation Project 1212010611809

the Basic Outlay of Scientific Research Work from Ministry of Science and Technology of the People's Republic of China J0803

SINOPPROBE-II, the Ministry of Land and Resources of China 2004DKA20280-2-5

Open Fund of Key Laboratory of Geo-detection (China University of Geosciences, Beijing) GDL0603

More Information
  • Corresponding author: Gao Rui, gaorui@cags.net.cn
  • Received Date: 25 Nov 2008
  • Accepted Date: 25 Jan 2009
  • The Qinghai (青海)-Tibet plateau is the newest and biggest orogenic belt in the world and a natural laboratory for researching continental geodynamics, such as continent-continent collision, convergence, subduction, and plateau uplift. From the 1950s to the present, there have been many active-source (deep seismic sounding and deep seismic reflection profiling) and passive-source seismic probing (broadband seismic observations) implemented to reveal the crust-mantle structure. In this article, the authors mainly summarize the three seismic probings to discuss the Moho depth of the Qinghai-Tibet plateau based on the previous summaries. The result shows that the Moho of the Qinghai-Tibet plateau is very complex and its depth is very different; the whole outline of it is that the Moho depth is deeper beneath the south than the north and deeper in the west than in the east. In the Qiangtang (羌塘) terrane, the hinterland of the Qinghai-Tibet plateau, the Moho is shallower than both the southern and the northern sides. The deepest Moho is 40 km deeper than the shallowest Moho. This trend records the crustal thickening and thinning caused by the mutual response between the India plate and the Eurasia plate, and the eastward mass flow in the Qinghai-Tibet plateau.

     

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