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《Chinese Journal of Geophysics》 1986-05
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SEISMIC TOMOGRAPHY OF NORTH CHINA REGION

LIU FU-TIAN QU KE-XIN WU HUA LI QIANG LIU JIAN-HUA HU GE 1) Institute of Geophysics, Academia Sinica, Beijing.27 Institute of Geophysics, State Seimological Bureau, Beijing.  
By using 7520 P arrivals recorded in the North China region (110.5°E-123.0°E, 30.5°N-41.5°N) during the period from 1981 to 1984, we have reconstructed the 3-D velocity structures of the crust and uppermost mantle of the, region with the orthogonal projection method, and graphed the velocity cross-sections of various depths (horizontal cross-section) with digital image processing technique. The results of tomography demonstrate that 1. there is significant lateral inhomogeneity in wave velocity in the North China region; 2. nearly all the strong earthquakes occur in the transition zones between high velocity regions and low velocity regions; 3, the image of the velocity cross-section of 14 km depth is very similar to that of well-known geological structure, and there are three significant low velocity regions on the velocity cross-section of 75 km depth, located respectively at Tan-Lu fault zone, Taihang mountain piedmont fracture zone and the Shanxi depression fault zone. This result is favorable to the assumption that the above-mentioned regions are continental rift valley zones.While reconstructing the 3-D velocity structure, we have carefully relocated hypo-centers of 129 earthquakes in the region.
【Fund】: 中国科学院科学基金的资助
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