中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Surface deformation related to the 2008 Wenchuan earthquake, and mountain building of the Longmen Shan, eastern Tibetan Plateau

文献类型:期刊论文

作者Fu, Bihong1; Shi, Pilong1; Guo, Huadong2; Okuyama, Satoshi3; Ninomiya, Yoshiki3; Wright, Sarah4
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2011-03-03
卷号40期号:4页码:805-824
关键词M-s 8.0 Wenchuan Earthquake Co-seismic Oblique Reverse Faulting Crustal Shortening Mountain Building Longmen Shan Eastern Tibetan Plateau
ISSN号1367-9120
DOI10.1016/j.jseaes.2010.11.011
文献子类Article
英文摘要The 12 May 2008 M-s 8.0 Wenchuan earthquake, China, was one of largest continental thrusting events worldwide. Based on interpretations of post-earthquake high-resolution remote sensing images and field surveys, we investigated the geometry, geomorphology, and kinematics of co-seismic surface ruptures, as well as seismic and geologic hazards along the Longmen Shan fold-and-thrust belt. Our results indicate that the Wenchuan earthquake occurred along the NE-SW-trending Yingxiu-Beichuan and Guanxian-Anxian faults in the Longmen Shan fold-and-thrust belt. The main surface rupture zones along the Yingxiu-Beichuan and Guanxian-Anxian fault zones are approximately 235 and 72 km in length, respectively. These sub-parallel ruptures may merge at depth. The Yingxiu-Donghekou surface rupture zone can be divided into four segments separated by discontinuities that appear as step-avers or bends in map view. Surface deformation is characterized by oblique reverse faulting with a maximum vertical displacement of approximately 10 m in areas around Beichuan County. Earthquake-related disasters (e.g., landslides) are linearly distributed along the surface rupture zones and associated river valleys.
WOS关键词AMBIENT SEISMIC NOISE ; WAVE ARRAY TOMOGRAPHY ; LOWER CRUSTAL FLOW ; GEOLOGICAL STRUCTURES ; 2-STATION ANALYSIS ; NORTHERN TIBET ; SICHUAN BASIN ; SLIP FAULTS ; SE TIBET ; CHINA
WOS研究方向Geology
语种英语
WOS记录号WOS:000287950800002
出版者PERGAMON-ELSEVIER SCIENCE LTD
源URL[http://ir.iggcas.ac.cn/handle/132A11/73560]  
专题中国科学院地质与地球物理研究所
通讯作者Fu, Bihong
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Ctr Earth Observat & Digital Earth, Beijing 100080, Peoples R China
3.Geol Survey Japan, AIST, Tsukuba, Ibaraki 3058567, Japan
4.Univ Melbourne, Sch Earth Sci, Melbourne, Vic 3010, Australia
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Fu, Bihong,Shi, Pilong,Guo, Huadong,et al. Surface deformation related to the 2008 Wenchuan earthquake, and mountain building of the Longmen Shan, eastern Tibetan Plateau[J]. JOURNAL OF ASIAN EARTH SCIENCES,2011,40(4):805-824.
APA Fu, Bihong,Shi, Pilong,Guo, Huadong,Okuyama, Satoshi,Ninomiya, Yoshiki,&Wright, Sarah.(2011).Surface deformation related to the 2008 Wenchuan earthquake, and mountain building of the Longmen Shan, eastern Tibetan Plateau.JOURNAL OF ASIAN EARTH SCIENCES,40(4),805-824.
MLA Fu, Bihong,et al."Surface deformation related to the 2008 Wenchuan earthquake, and mountain building of the Longmen Shan, eastern Tibetan Plateau".JOURNAL OF ASIAN EARTH SCIENCES 40.4(2011):805-824.

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来源:地质与地球物理研究所

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