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SIMULATION OF THE SEISMIC TECTONIC STRESS FIELD IN NORTH CHINA

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【作者】王仁；黄杰藩；孙荀英；安欧；郭世凤；宋惠珍；潘善德；黄庆华；沈淑敏；杨建华；

【Author】 WANG REN;HUANG JIEFAN;SUN XUNYING;AN OU;GUO SHIFENG;SONG HUIZHEN;PAN SHANDE;HUANG QINGHUA;SHEN SHUMIN;YANG JIANHUA Peking University Seismo-geological Team, State Seismological Buream, Beijing Institute of Geology, State Seismological Bureau, Beijing Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing Geological Team No. 562, Ministry of Geology, Hebei Province

【机构】 Peking University； Seismo-geological Team； State Seismological Buream； Beijing； Institute of Geology； State Seismological Bureau； Institute of Geomechanics； Chinese Academy of Geological Sciences； Geological Team No. 562； Ministry of Geology； Hebei Province；

【摘要】 <正> The paper reviews several methods of simulation used in this country to recover currenttectonic stress field related to earthquake occurrence in North China. The aim is to evaluatethe degree of seismic risk around Beijing area. The methods used are computational ormathematical simulation by the finite element method and experimental or physical simulationby the photoelastic method and the grid method. The results obtained by these methods arebriefly described. Most simulations indicate that Beijing is not a region of seismic risk.更多还原

【Abstract】 The paper reviews several methods of simulation used in this country to recover currenttectonic stress field related to earthquake occurrence in North China. The aim is to evaluatethe degree of seismic risk around Beijing area. The methods used are computational ormathematical simulation by the finite element method and experimental or physical simulationby the photoelastic method and the grid method. The results obtained by these methods arebriefly described. Most simulations indicate that Beijing is not a region of seismic risk.更多还原

【关键词】 recover； satisfactory； umber； fitting； outside； strata； slight； latter； rotation； fitted；

【文献出处】 Science in China,Ser.B ,中国科学B辑(英文版) , 编辑部邮箱 ,1982年09期

【被引频次】1
【下载频次】68

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