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《Chinese Journal of Geophysics》 1993-03
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3-D SHEAR VELOCITY STRUCTURE IN NORTH-WEST CHINA

AN CHANG-QIANG SONG ZHONG-HE CHEN GUO-YING CHEN LI-HUA(Institute of Geophysics, State Seismological Bureau, Beijing 100081)ZHUANG ZHEN Fu ZHU-WU Lu ZHI-LING Hu JIA-FU(Department of Geophysics,Yunnan University, Kunming 650091)  
Different tectonic units in North-West China, such as Junggar Basin, Altay Mt., Tian-shan Mt., Inner-Mongolian Fold Zone, Tarim Basin, Qaidam Basin and Qilian Mt., are discussed in the present study. It is found out based on the group velocity of Rayleigh wave and the relevant models of shear wave velocity in depth that Tarim Basin shows certain distinct features of a stable geological block, while other tectonic units belong to active areas. Their particular velocity distribution in depth are related to their tectonic evolution. A considerable portion of Bouguer gravity anomaly is contributed by the relief of Moho discontinuity. It is also found out that there exist obvious difference in velocity structure between eastern part (Beishan) and western part of Tianshan in the lid of the upper mantle. The high velocity lid in the upper mantle is related to the special stress field in this area.
【Fund】: 国家自然科学基金
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