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《Chinese Journal of Geophysics》 1997-05
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THREE-DIMENSIONAL LITHOSPHERIC DENSITY STRUCTURE BENEATH QINGHAI-TIBET AND ITS ADJACENT AREA

FANG JIAN; XU HOU-ZE (Institute of Geodesy and Geophysics, Academia Sinica, Wuhan, 430077, China)  
We have abtained more than 20 000 practical gravity data and three-dimensional tomographic inversion results of shear velocity in Qinghai-Tibet (QT) region. Firstly, we made up initial model of lihospheric density of QT region using the empirical equation between the density difference and shear velocity difference. Then, inversion of 30'×30' Bouguer gravity anomaly by means of Marquardt-leverberg method yield a rather detailed density structural model. The results indieate as follows: (1) Lithospheric density distribution are inhomogeneous not only in vertical direction but aslo in horizontal direction, In the depth 10-70km ranges, QT plateau appears lower density. In the depth 50-70km ranges QT plateau more lower than its adjacent region,has 0.1g /cm3 density difference; In 90-110km depth ranges QT platean lithospheric mantle appears high density character. (2) the Lithospheric density distribution is relative with geotectonics, there are QT block, Bayancla block, Tarim biock and Indian block.
【CateGory Index】: P631.4
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