中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Parameter inversion of the 1997 mani earthquake from insar co-seismic deformation field based on linear elastic dislocation model - i. uniform slip inversion

文献类型:期刊论文

作者Sun Jian-Bao; Xu Xi-wei; Shen Zheng-Kang; Shi Yao-Lin; Liang Fang
刊名Chinese journal of geophysics-chinese edition
出版日期2007-07-01
卷号50期号:4页码:1097-1110
关键词Mani earthquake Sar interferometry Co-seismic deformation Linear elasticity Uniform slip inversion Distributed slip inversion
ISSN号0001-5733
通讯作者Sun jian-bao(suninsar@yahoo.com)
英文摘要The nov. 8, 1997 mani (xizang) mw7.5 earthquake is an important event since synthetic aperture radar lnterferometry was used for earthquake studies. peltzer et al argued that the deformation field indicated the nonlinear elastic response of crust with a ratio of 2 between compressive and tensile elastic moduli. no other similar case appeared in co-seismic deformation field. generally, linear elastic theory can give satisfactory explanation to the observation. considering their excessively simplified fault model and the pure strike-slip assumption, we deem that nonlinear elasticity explanation is far-fetched. by using the widely-used okada linear elastic dislocation model and the fault location on the surface from satellite observations, removing the zero dip-slip constraint, we seek best-fit fault geometry parameters and uniform slip vectors from radar observation based on nonlinear optimization inversion. the result shows that linear elastic model can satisfactorily explain the observation. the maximum depth of the fault reaches 16.5 km at the segment near the east side of chaoyang lake. the depth decreases gradually when the fault extending to the east and the west; inverted fault dipping direction and dip-slip are consistent with field investigation; the maximum strike-slip component reaches 4.44 m, and the dip-slip component also reaches its maximum 1.1 m at this segment, which can not be ignored in the inversion; the total seismic moment is 2.08 x 10(20) n . m from inversion, which equals to a mw7.5 earthquake. the seismic moment is close to the 2.23 x 10(20) n . m of harvard solution and the 1.8 x 10(20) n . m of velasco's inversion.
WOS关键词RADAR INTERFEROMETRY ; KUNLUN FAULT ; DISPLACEMENT FIELD ; HECTOR MINE ; SURFACE ; CHINA ; TIBET ; CALIFORNIA ; SPACE ; GPS
WOS研究方向Geochemistry & Geophysics
WOS类目Geochemistry & Geophysics
语种英语
WOS记录号WOS:000248343500017
出版者SCIENCE CHINA PRESS
URI标识http://www.irgrid.ac.cn/handle/1471x/2383558
专题中国科学院大学
通讯作者Sun Jian-Bao
作者单位1.Chinese Acad Sci, Grad Univ, Sch Earth Sci, Beijing 100049, Peoples R China
2.China Earthquake Adm, Inst Geol, Beijing 100029, Peoples R China
3.Chinese Acad Sci, Beijing Earthquake Adm, Beijing 100080, Peoples R China
推荐引用方式
GB/T 7714
Sun Jian-Bao,Xu Xi-wei,Shen Zheng-Kang,et al. Parameter inversion of the 1997 mani earthquake from insar co-seismic deformation field based on linear elastic dislocation model - i. uniform slip inversion[J]. Chinese journal of geophysics-chinese edition,2007,50(4):1097-1110.
APA Sun Jian-Bao,Xu Xi-wei,Shen Zheng-Kang,Shi Yao-Lin,&Liang Fang.(2007).Parameter inversion of the 1997 mani earthquake from insar co-seismic deformation field based on linear elastic dislocation model - i. uniform slip inversion.Chinese journal of geophysics-chinese edition,50(4),1097-1110.
MLA Sun Jian-Bao,et al."Parameter inversion of the 1997 mani earthquake from insar co-seismic deformation field based on linear elastic dislocation model - i. uniform slip inversion".Chinese journal of geophysics-chinese edition 50.4(2007):1097-1110.

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来源:中国科学院大学

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