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《Chinese Journal of Geophysics》 1991-03
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A SEISMIC SOURCE MODEL OF THE LARGE EARTHQUAKES IN NORTH CHINA EXTENSIONAL BASIN AND DISCUSSIONS ON THE GENETIC PROCESSES OF THE EXTENSIONAL BASIN AND EARTHQUAKES

ZENG RONG-SHENG ZHU LU-PFI HE ZHENG-QING DING ZHI-FENG SUN WEI-GUO(Institute of Geophysics, State Seismological Bureau, Beijing, 100081)  
Since the Tertiary, numerous intervening depressions and upliftings have been produced in the North China Basin due to the differential sinking of the Basin. The North China Basin can not be interpreted properly with the thermal-rifting and the pull-apart models. A broken Moho was observed near the epicemral area of Tangshan earthquake from DSS result, and a prominent low velocity zone extending from the uppermost mantle to the middle crust was found near the epicentral area from 'he results of seismic computerized tomography. They indicate that a magmatic body of high temperature had penetrated form the uppermost mantle to the middle crust through the broken Moho. A new model for interpreting the seismoge-netic process and the generation of depressions in the upper part of the crust is suggested by the authors of present paper. A smaller stress field due to the injection of magma from the uppermost mantle to the middle crust is produced in addition to the horizontal tectonic stress field, which is more uniform in a large-scale area. The disturbance due to the injected magma varies in both lateral and vertical directions. It produces a considerably large ex-Tensional force in the upper part of the crust and a horizontal shear stress in the middle and lower parts of the crust at the same time. This model also avoids the difficulty that the cru-stal thickness doesn't decrease, while the heat flow is high in North China Basin.Since the rheology varies with the depth, a two-level seismic source of a large earthquake may comprise a brittle deformation in the upper part of the crust and a ductile deformation in the middle or even the lower curst.
【Fund】: 地震科学联合基金
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