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The ground deformation field induced by a listric thrust fault with an overburden soil layer
Zeng, Shaogang ; Cai, Yong&apos ; en
刊名frontiers of earth science
2013
关键词listric thrust fault earthquake fault scarps ground fissures finite element method (FEM) RUPTURE PROPAGATION SURFACE RUPTURE TENSILE FAULTS HALF-SPACE DISPLACEMENT EARTHQUAKE SLIP SHEAR
DOI10.1007/s11707-013-0383-x
英文摘要The surface deformation field induced by a listric thrust fault with a thick, overburden soil layer is studied in this paper by the finite element method (FEM). The results show: (a) The maximum slip induced by the buried fault is not located at upper tip of the fault, but below it. (b) The vertical displacement changes remarkably near the fault, forming a fault scarp. With the increase of the soil layer thickness, the height of the scarp is decreased for the same earthquake magnitude. (c) The strong strain zone on the surface is localized near the projection of the fault tip on the ground surface. The horizontal strains in the zone are in tension above the hanging wall and in compression above the foot wall, and the vertical strains in the zone are vice versa, which is favorable for tensileshear, compression-shear fissures above hanging wall and foot wall, respectively.; Geosciences, Multidisciplinary; SCI(E); 中国科技核心期刊(ISTIC); 中国科学引文数据库(CSCD); 0; ARTICLE; 4; 501-507; 7
语种英语
内容类型期刊论文
源URL[http://ir.pku.edu.cn/handle/20.500.11897/311062]  
专题地球与空间科学学院
推荐引用方式
GB/T 7714
Zeng, Shaogang,Cai, Yong&apos,en. The ground deformation field induced by a listric thrust fault with an overburden soil layer[J]. frontiers of earth science,2013.
APA Zeng, Shaogang,Cai, Yong&apos,&en.(2013).The ground deformation field induced by a listric thrust fault with an overburden soil layer.frontiers of earth science.
MLA Zeng, Shaogang,et al."The ground deformation field induced by a listric thrust fault with an overburden soil layer".frontiers of earth science (2013).
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