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《Chinese Journal of Geophysics》 1999-02
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3-D CRUST AND UPPER MANTLE VELOCITYSTRUCTURE IN EASTERN TIBETAN PLATEAU AND ITSSURROUNDING AREAS

DING ZHI-FENG; HE ZHENG-QIN; SUN WEI-GUO(Institute of Geophysics, China Seismological Bureau, Beijing 100081, China)SUN HONG-CHUAN(Department of Geology and Geophysics, Utah University, Utah 84112-1183, USA)  
Over 10000 arrival time data of local seismic events recorded in Tibetan Plateauand its surrounding areas were used to inverse 3-D crust and upper mantle velocitystructure. The 3-D velocity structure was described by grid point model, with thedimension of 22 22 6. The intervals of grid points are 100km in horizontal and20km in vertical. The velocity value among grid points were given by interpolation.An advanced fast 3-D ray tracing method was used to determine the seismic raypaths and synthetic arrival times in 3-D inhomogeneous media. The results show thatthere is a low velocity zone in the upper crust (about 30km depth) of southem Tibet,which is coincident with the results from surface wave invereion; there is an evidentlow velocity zone in the lower crust of Qiangtang block; The vertical velocity profilealong Qinghai-Tibet highway demonstrates the structure characteristics of thecompressed and deepened lithosphere.
【Fund】: 地震学联合基金!94021
【CateGory Index】: P313
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