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《Chinese Journal of Geophysics》 1989-01
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PRELIMINARY STUDY OF UPPER MANTLE SHEAR VELOCITY STRUCTURE OF CHINA

WANG KAI YAO ZHEN-XING(Institute of Geophysics, Academia Sinica, Beijing)  
In this paper SS-S travel times and SS waveforms have been used to study the upper mantle shear velocity structure of China by modeling SH synthetic seismograms. We primarily divide China continent into two different regions. The one is Qinghai-Tibet plateau, and the another is eastern part of China continent. There are low velocity zones (LVZ) in these two regions, but the depths of LVZ are different. The depth is 100 km for plateau, 60 km for eastern region, and the difference of two regions gradually disappear below the 350 km. The two regions have first order discontinuities of shear velocity at 405 km and 660 km. Below 400 km, the shear velocity structure of China is the same as in North America, Northwest of Atlantic Ocean, Europe and Alpine belt. This result shows that there are little heterogeneity of upper, mantle shear velocity below 400 km between these regions.
【Fund】: 中国科学院基金
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