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《Chinese Journal of Geophysics》 1991-04
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THREE-DIMENSIONAL SHEAR VELOCITY STRUCTURE BENEATH QINHAI-TIBET AND ITS ADJACENT AREA

ZHOU BIN ZHU JIE-SHOU(Chengdu College of Geology, Chengdu 610059)CHUN KIN-YIP(University of Toroto, Canada)  
Surface wave data, consisting of 140 individual dispersion curves, have been obtained from 13 stations located in and outside of the Qinhai-Tibet region of western China. Tomographic inversion of the data have yeilded a rather detailed structural model (10-110 km depth range) beneath the studied region. The results indicate as follows: (1) The study region consists of four distinct crust-mantle velocity substructures, each of which can be identified with one of the known tectonic units: Qinghai-Tibet block, Chaidamo-Bayarhar/Three River block, Ta-rim block and the Indian subcontinent. The average lithospheric velocity is lowest beneath the Qinhai-Tibet region and the highest beneath the Tarim block. (2) At the depth exceeding 70 km, the Moho discontinuity in north of Yarlung Zangbo river reaches the deepest point of a "basin" configuration, whose marginal depth is about 50 km. (3) The Tibetan crustal s'ruc-ture resembles a vertically stretched out model of the Indian subcontinent. (4) Pangong Lake Fault and Nujiang Jinsha River Fault are deep-rooted structural features along which the Moho discontinuity suffers a vertical offset, with ihe northeastern side being relatively shallower. (5) The velocity structure within the Chaidamo-Bayarhar/Three River block is laterally in-homogeneous. Ranging from 90 to 110 km, the upper mantle low velocity layer in this region is more prominent as well as shallower than that beneath the Qinhai-Tibet plateau- And (6) the velocity increases monotonically with depth beneath the stable Tarim Basin block where the crust is about 50 km thick.
【Fund】: 地震科学联合基金
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