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《Chinese Journal of Geophysics》 1983-03
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THE STRESS RELEASE AND ADJUSTMENT PROCESS DURING TANGSHAN EARTHQUAKE SEQUENCE

LI QIN-ZU DIAO GUI-LING DAI YING-HUA(Seismological Bureau of Hebei Province)  
The first motion data for the sequence of earthquakes with Ms≥4.0 during the period Jul. 28, 1976-Dee. 31, 1979 after the Tangshan earthquake were gathered from readings of seismograms for 68 stations and from bulletin for other 14 stations. The reliable fault plane solutions for 167 earthquakes were obtained. The analysis of these FPS shows that there was a stress release and adjustment process in the source region during the Tangshan earthquake sequence. The process developed gradually from an equilibrium state before the main shock to another equilibrium state, via an extremely unstable state after the main shock; and the detail of the process is different for various parts of the aftershock area. The orientations of principal axes in the two equilibrium states are approximately the same. It implies that principal features of the tectonic stress field of the Tangshan region are not redically changed after the earthquake. Therefore the tectonic movement of this region will continue it's course and the same seismic activity will prevail in the future.
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