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《Chinese Journal of Geophysics》 2008-04
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Slip rates and recurrence intervals of the Longmen Shan active fault zone,and tectonic implications for the mechanism of the May 12 Wenchuan earthquake,2008,Sichuan,China

ZHANG Pei-Zhen~1 XU Xi-Wei~1 WEN Xue-Ze~2 RAN Yong-Kang~1 1 State Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration,Beijing 100029,China 2 Sichuan Seismological Bureau,Chengdu 610041,China  
The great Wenchuan earthquake of May 12,2008 occurs on the Longmen Shan fault zone which forms a prominent section of the seismically very active seismic belt called the North- South Trending Seismic Belt by Chinese seismologists.There have been 3 earthquakes with magmtudes from 6 to 61/2 along the Longmen Shan fault zone during more then 2000 year documented history of the Sichuan province.Previous active faulting studies indicate slow(less than 3 mm/yr)slip rate across the Longmen Shan fault zone.Why such a strong earthquake occurred in the Longmen Shah fault zone?What are the characteristics of the May 12 earthquake? What is the tectonic mechanism of the earthquake?On the basis of geological studies of the earthquake surface rupture zone and pre-earthquake GPS measurements in the region,we try to understand the questions mentioned above.The May 12 earthquake,2008 is caused by displacement along the Yingxiu-Beichuan fault along which a more than 200 km long surface ruptures was formed.Another strand of the Longmen Shan fault zone,Guanxian-Jiangyou fault also ruptured as indicated by more then 60 km long surface ruptures.GPS measurements before the earthquake suggest that slip rate across the entire Longmen Shan fault zone does not excess about 2 mm/yr,and does not excess 1 mm/yr across individual fault strand.These data agree with seismogeological studies and historical seismicity of the Sichuan province.Using maximum coseismic displacement obtained from seismogeological studies and inversions from seismic waves, the recurrence intervals of great earthquakes,such as the 2008 Wenchuan earthquake,can be estimated to be 2000~6000 years.The Longmen Shan fault zone has a high dipping angle(more than 50°~60°)near surface and low-angle at depth(15~20 kin).This kind of listric shape favors significant strain or energy accumulation to form great earthquake.The May 12 Wenchuan earthquake,2008 is characterized by slow strain accumulation,long recurrence interval,and significant damage power.It is a new type of earthquake event that deserves further studies.
【Fund】: 国家重点基础研究发展规划(973)项目(2004CB418400)资助
【CateGory Index】: P315
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7 SUN Xiao-meng,DU Ji-yu,SHAN Xuan-long,CHENG Ri-hui,WANG Ying-de,XU Qiang-wei,TIAN Jing-xiongCollege of Earth Sciences,Jilin University,Changchun 130026,China;Tectonic Zonation of Front Range and Deformation Features of Foreland in Northern Longmen Mountain Thrust Zone[J];Journal of Jilin University(Earth Science Edition);2010-06
8 LI Li-li College of Geo-Exploration Science and Technology,Jilin University,Changchun 130026,China;Variation Features of Gravity Anomaly in Wenchuan Area Before and After Earthquake[J];Journal of Jilin University(Earth Science Edition);2011-S1
9 Ma Guo-qing,Meng Ling-shun,Li Li-li College of GeoExploration Science and Technology,Jilin University,Changchun 130026,China;Fault Distribution of Longmenshan and Adjacent Regions and Fault Morphological Differences Before and After the Earthquake[J];Journal of Jilin University(Earth Science Edition);2012-02
10 CAO Jun-xing1,2,LIU Shu-gen1,HE Xiao-yan2,ZHAO Liang2 1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China 2.College of Information Engineering,Chengdu University of Technology,Chengdu 610059,China;Dynamic coupling mechanism between Longmenshan and Sichuan Basin and its impact on the hydrocarbon migration in West Sichuan based on the analysis of the characteristics of Wenchuan earthquake[J];Journal of Chengdu University of Technology(Science & Technology Edition);2009-06
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1 Zuan Chen~(a,c,*),Banghui Lin~b,Wuming Bai~a,Xu Cheng~a,Yunsheng Wang~c a Key Laboratory of the Study of Earth's Deep Interior,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China b Institute of Geophysics,Chinese Seismological Bureau,Beijing 100081,China c State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,Chengdu University of Technology,Chengdu,610059,China;A study on the influence of the 2008 Wenchuan earthquake on the stability of the Qinghai-Tibet Plateau tectonic block system[A];[C];2012
2 CHEN Zu-An~(1,3),LIN Bang-Hui~2,BAI Wu-Ming~1,CHENG Xu~1,WANG Yun-Sheng~3 1 Key Laboratory of the Study of Earth's Deep Interior,Institute of Geology and Geophysics,The Chinese Academy of Sciences, Beijing 100029,China 2 Institute of Geophysics,Chinese Seismological Bureau,Beijing 100081,China 3 State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,Chengdu University of Technology, Chengdu 610059,China;A study on the rupture process of the 2001 Ms8.1 Kunlunshan earthquake and its influence on pregnant process and occurrence of the Ms8.0 Wenchuan earthquake in 2008[A];[C];2012
3 F.C.Dai~(a,*),X.B.Tu~a,C.Xu~a,Q.M.Gong~b,X.Yao~c a Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing 100029,PR China b College of Architecture and Civil Engineering,Beijing University of Technology,Beijing 100022,PR China c Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,PR China;Rock avalanches triggered by oblique-thrusting during the 12 May 2008 Ms 8.0Wenchuan earthquake,China[A];[C];2012
4 SUN Chang-Qing~(1,2),CHEN Yun~(1*),GAO Er-Gen~3 1 Stale Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences, Beijing 100029,China 2 Graduate University of Chinese Academy of Sciences,Beijing 100049,China 3 Department of Seismology Science,Institute of Disaster Prevention Science and Technology,Yanjiao Town, Hebei Province 065201,China;The crustal anisotropy and its geodynamical significance of the strong basin-range interaction zone beneath the east margin of Qinghai-Tibet plateau[A];[C];2012
5 ZHOU Jian~(1,2),ZHANG Luqing~1,HURuilin~1,WANG Xueliang~(1,2) (1.Key Laboratory of Engineering Geomechanics,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China);STUDY OF RULES OF STRESS WAVES PROPAGATION UNDER VARIOUS ATTITUDES OF LARGE-SCALE FRACTURES[A];[C];2012
6 LI ZhiWei~(1*),Xu Yi~1,Huang RunQiu~2,Hao TianYao~1,Xu Ya~1,Liu JingSong~1 & Liu JianHua~1 Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics,Chinese Academy of Sciences, Beijing 100029,China; State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,Chengdu University of Technology,Chengdu 610059,China;Crustal P-wave velocity structure of the Longmenshan region and its tectonic implications for the 2008 Wenchuan earthquake[A];[C];2012
7 CHEN Houqun(China Institute of Water Resources and Hydropower Research,Beijing 100038,China);The Seismic Safety of the Three Gorges Dam and Reservoir Seismic[A];[C];2009
8 BO Wanju(First Crust Deformation Monitoring and Application Center,Tianjin 300180,China);Mainly Relative Deformation Features on China Continent Revealed by GPS and Researches on Strong Earthquake Activities[A];[C];2011
9 FU BiHong,WANG Ping,KONG Ping,ZHENG GuoDong,WANG Gang and SHI PiLong 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.State Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration,Beijing 100029,China 3.Chengdu University of Technology,Chengdu 610059,China;Preliminary study of coseismic fault gouge occurred in the slip zone of the Wenchuan Ms 8.0 earthquake and its tectonic implications.[A];[C];2009
10 TENG Ji-Wen Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Ponder and research on the genesis and occurrence of strong earthquakes and the prediction of their place,time and intensity[A];[C];2011
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