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《Chinese Journal of Geophysics》 1992-06
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3-D SHEAR VELOCITY MODEL OF CRUST AND UPPER MANTLE BENEATH THE TIBETAN PLATEAU AND ITS ADJACENT REGIONS

ZHUANG ZHEN Fu ZHU-WU Lu ZI-LING Hu JIA-FU(Yunnan University, Kunming 650091)SONG ZHONG-HE CHEN GUO-YING AN CHANG-QIANG CHEN LI-HUA(Institute of Geophysics, State Seismological Bureau, Beijing 100081)  
In the present study, 238 long-period surface wave records from 30 seismic network stations are selected, Matched-Filtering and Grid Dispersion Inversion are performed on these data to give the Rayleigh pure-path dispersion curves ranging from 10 to 105 seconds for 147 composing grids of China and the adjacent area, then the 3-D shear velocity model of the crust and upper mantle beneath the Tibetan Plateau and its adjacent regions to a depth of 170km is in-versed. It is found that: the average crust thicknesses of the Mid-Western and Eastern Tibetan Plateau are 70 ±7km and 65±7km respectively, the average shear velocities Vs in the crusts of the two areas are 3.55km/s and 3.62km/s re spectively, the average Vs of the lid in the upper mantle of the two areas are 4.63km/s and 4.61km/s respectively. The thickness of the li-thosphere of the Tibetan Plateau is about 120±10km. There are extensive low velocity layers in the lower crust of depth from 30 to 40km in the eastern part of the Plateau. There exists a well-observed swelling-up low velocity channel within the upper mantle low velocity zone beneath the Tibetan Plateau and its eastern flank. In the area of the western Yunnan and northern Burma the crust thickness is 45 ±5km, there are low velocity layers in both the lower and upper crusts, and Vs of the lid in the upper mantle is 4.42km/s which is less than tha± in the Tibetan Plateau and in the Ganges area. In Ganges area the crust thickness is 34± 2km, the crustal Vs is 3.45 km/s, the lid thickness of the upper mantle is 86 ±10km, Vs of the lid is 4.63km/s, within the lid there is an inserted low velocity section of depth from 55 km to 83 km.
【Fund】: 国家自然科学基金
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