SPATIAL RELATIONSHIPS BETWEEN SURFACE RUPTURES IN THE Ms 8.0 WENCHUAN EARTHQUAKE, THE LONGMEN SHAN REGION, SICHUAN, CHINA

被引:7
|
作者
Li Yong [1 ]
Zhou Rongjun [2 ]
Densmore, Alexander L. [3 ,4 ]
Cao Shuyou [5 ]
Liu Yuping [6 ]
机构
[1] Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Sichuan, Peoples R China
[2] Seismol Bur, Inst Earthquake Engn, Chengdu 610041, Sichuan Provinc, Peoples R China
[3] Univ Durham, Inst Hazard Risk & Resilience, Durham, England
[4] Univ Durham, Dept Geog, Durham, England
[5] Sichuan Univ, State Key Lab Hydraul & Mt River Engn, Chengdu 610064, Sichuan, Peoples R China
[6] Chengdu Inst Geol & Mineral Resources, Chengdu 610081, Sichuan, Peoples R China
基金
中国国家自然科学基金;
关键词
Surface ruptures; Wenchuan Earthquake; Longmen Shan region; LOWER CRUSTAL FLOW; TIBETAN PLATEAU; EASTERN MARGIN; DEFORMATION; BASIN; FAULT; BELT; KINEMATICS; UPLIFT;
D O I
10.1142/S1793431111001121
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
During the M-s 8.0 Wenchuan Earthquake of May 12, 2008, three distinct faults in the Longmen Shan along the eastern margin of the Tibetan Plateau ruptured. We have carried out detailed field geological mapping on these faults (the Yingxiu-Beichuan, the Pengxian-Guanxian, and the Xiaoyudong Faults), as well as the minor Leigu Fault, using GPS and total station surveys. The surface rupture of the Wenchuan Earthquake consists of two margin-parallel thrust faults linked by the Xiaoyudong tear fault. By comparing the features of the surface rupture of the faults, the spatial relationships between the different surface ruptures can be determined. It is clear that the margin-parallel thrust faults are linked at depth, forming an imbricated thrust linked by a tear fault.
引用
收藏
页码:329 / 342
页数:14
相关论文
共 50 条
  • [31] Rupture process of the Wenchuan M8.0 earthquake of Sichuan China: the segmentation feature
    Zhao CuiPing
    Chen ZhangLi
    Zhou LianQing
    Li ZhiXiong
    Kang Yin
    CHINESE SCIENCE BULLETIN, 2010, 55 (03): : 284 - 292
  • [32] Rupture process of the Wenchuan M8.0 earthquake of Sichuan, China: the segmentation feature
    ZHAO CuiPing1
    2China Earthquake Administration
    3Seismological Bureau of Guangdong Province
    Science Bulletin, 2010, (03) : 284 - 292
  • [33] Rupture process of the Wenchuan M8.0 earthquake of Sichuan, China: the segmentation feature
    ZHAO CuiPing CHEN ZhangLi ZHOU LianQing LI ZhiXiong KANG Yin Insitute of Earthquake Science China Earthquake Administration Beijing ChinaChina Earthquake Administration Beijing ChinaSeismological Bureau of Guangdong Province Guangzhou China
    Chinese Science Bulletin, 2010, 55 (03) : 284 - 292
  • [34] The M7.0 Lushan earthquake and the relationship with the M8.0 Wenchuan earthquake in Sichuan, China
    Du Fang
    Long Feng
    Ruan Xiang
    Yi Gui-Xi
    Gong Yue
    Zhao Min
    Zhang Zhi-Wei
    Qiao Hui-Zhen
    Wang Zhi
    Wu Jiang
    CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, 2013, 56 (05): : 1772 - 1783
  • [36] Abnormal Phenomena Recorded by Several Earthquake Precursor Observation Instruments Before the Ms 8.0 Wenchuan, Sichuan Earthquake
    Ouyang Zuxi
    Zhang Hongxun
    Fu Zizhong
    Gou Bo
    Jiang Wali
    ACTA GEOLOGICA SINICA-ENGLISH EDITION, 2009, 83 (04) : 834 - 844
  • [37] Crustal motion of Chinese mainland and preparation of MS8.0 Wenchuan earthquake in Sichuan Province
    Guo Liang-Qian
    Li Yan-Xing
    Hu Xin-Kang
    Liu Xia
    CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, 2009, 52 (02): : 531 - 537
  • [38] Structural model of 2008 Mw 7.9 Wenchuan earthquake in the rejuvenated Longmen Shan thrust belt, China
    Jia, Dong
    Li, Yiquan
    Lin, Aiming
    Wang, Maomao
    Chen, Wei
    Wu, Xiaojun
    Ren, Zhikun
    Zhao, Yao
    Luo, Liang
    TECTONOPHYSICS, 2010, 491 (1-4) : 174 - 184
  • [39] Seismic properties of the Longmen Shan complex: Implications for the moment magnitude of the great 2008 Wenchuan earthquake in China
    Sun, Shengsi
    Ji, Shaocheng
    Wang, Qian
    Wang, Hongcai
    Long, Changxing
    Salisbury, Matthew
    TECTONOPHYSICS, 2012, 564 : 68 - 82