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《Chinese Journal of Geophysics》 1996-03
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CRUST STRUCTURES AND STRONG EARTHQUAKES IN THE BEIJING, TIANJIN, TANGSHAN AREA: II. S WAVE VELOCITY STRUCTURE

SUN RUO-MEI; ZHAO YAN-LAI; WU DAN 1) (InsTitutE of Geophysics, Academia Sinica, Beijing 100101, China) 2) (Center for Analysis and Prediction, State Seismological Bureau, Beijing 100036, China)  
By using of 21 927 S arrival times of 2516 events, which occurred within the Beijing, Tianjing and Tangshan areas during 1986-1993, we carried out tomographic inversion. The results are: 1. The projection places of strong earthquakes since 1000 year on the image of the lower crust distribut within low velocity blocks or in transitional zones between high and low velocity areas, especially at edges of low velocity blocks. 2. Under the hypocenter of the Tangshan earthquake there are high Vp/Vs values, which are suggestive of a partially molten volume. There is an evidence, that hot material is upwelling through a fault from Moho to the hypocenter. 3. The central part of the Huanghua depression has low Vp/Vs values, which inferring a geothermal system near the water-stream transition in concert with the observed high heat flow values. High Vp/Vs values in the Jizhong depression might be exhibited by partially molten magma bodies.
【Fund】: 国家地震局“八五”科技攻关项目
【CateGory Index】: P313.2
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