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《Northwestern Seismological Journal》 2001-01
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DYNAMIC EVOLUTION OF STRESS FIELD INVERTED BY USING DATA OF WELL WATER LEVEL BEFORE AND AFTER THE DATONG YANGGAO M S6.1 EARTHQUAKE

ZHANG Zhao dong 1, LIU Qing guo 2, LIU Tao 3, CHEN Dian run 1 (1.Seismological Bureau of Shandong Province,Jinan 250014,China; 2.Architectural Engineering Institute of Shandong Province,Jinan 250014,China; 3.Constructive Bank of Shandong  
Dynamic change of regional stress field before and after the Datong Yanggao earthquake is inverted by using data of well water level.In the inversion,the method inverting stress change in water bearing system in reference [1] is used.The results show that the zero value line of stress field crosses epicentral regions of the Datong M S6.1 and M S5.8 earthquakes.The stress field of periphery of the epicentral region transformed from positive stress into negative stress,and the value of the positive stress increased gradually before the earthquakes.After the earthquakes,the stress field is slow in change.
【CateGory Index】: P315.72
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