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DOI10.1016/j.tecto.2011.05.009
Three-dimensional finite element modeling of stress evolution around the Xiaojiang fault system in the southeastern Tibetan plateau during the past similar to 500 years
He, Jiankun; Xia, Wenhai; Lu, Shuangjiang; Qian, Huashan
通讯作者He, JK (通讯作者)
发表日期2011
ISSN0040-1951
EISSN1879-3266
起始页码70
结束页码85
卷号507期号:1-4
英文摘要The left-lateral strike-slip Xiaojiang fault system is a main boundary between the southeastern Tibetan Plateau and the South China Block, and accumulates several large (M>7) earthquakes in the past similar to 500 years and a dozen of moderate (5 7) earthquake ruptures occurred in the past similar to 500 years are simulated with split-node technique in seismogenic upper crust. We investigate the Coulomb failure stress changes mainly on vertical planes parallel to the different strands of the Xiaojiang fault system, and at the epicenters of large (M>7) earthquakes in the past similar to 500 years and of moderate (5 7) earthquakes that occurred in the past similar to 500 years both from their coseismic and postseismic effects, among which the postseismic effect results in the stressing rate being obviously accelerated near epicenters of the large (M > 7) earthquakes after their occurrence. Thus, the percentage of positive Coulomb failure stress changes of >0.01 MPa at the epicenters increases from similar to 37% to similar to 50% for the large (M>7) earthquakes, and from similar to 43% to similar to 64% for the moderate (5
关键词LOWER CRUSTAL FLOWSOUTHERN CALIFORNIAACTIVE DEFORMATIONLARGE EARTHQUAKESXIANSHUIHE FAULTYUNNAN PROVINCEKUNLUN FAULTSLIP RATESRED-RIVERCHINA
英文关键词Coulomb failure stress changes; Earthquake; Viscoelastic; Finite element modeling; Xiaojiang fault system
语种英语
WOS研究方向Geochemistry & Geophysics
WOS类目Geochemistry & Geophysics
WOS记录号WOS:000293322600006
来源期刊TECTONOPHYSICS
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/257847
推荐引用方式
GB/T 7714
He, Jiankun,Xia, Wenhai,Lu, Shuangjiang,et al. Three-dimensional finite element modeling of stress evolution around the Xiaojiang fault system in the southeastern Tibetan plateau during the past similar to 500 years[J]. 中国科学院青藏高原研究所,2011,507(1-4).
APA He, Jiankun,Xia, Wenhai,Lu, Shuangjiang,&Qian, Huashan.(2011).Three-dimensional finite element modeling of stress evolution around the Xiaojiang fault system in the southeastern Tibetan plateau during the past similar to 500 years.TECTONOPHYSICS,507(1-4).
MLA He, Jiankun,et al."Three-dimensional finite element modeling of stress evolution around the Xiaojiang fault system in the southeastern Tibetan plateau during the past similar to 500 years".TECTONOPHYSICS 507.1-4(2011).
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