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《Seismology and Geology》 2008-03
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PRIMARY ANALYSES OF IN-SITU RECURRENCE OF LARGE EARTHQUAKE ALONG SEISMOGENIC FAULT OF THE M_S8.0 WENCHUAN EARTHQUAKE

RAN Yong-kang CHEN Li-chun CHEN Gui-hua YIN Jin-hui CHEN Jie GONG Hui-ling SHI Xiang LI Chen-xia(National Centre of Active Fault Studies,Institute of Geology,China Earthquake Administration,Beijing 100029,China)  
In the historical rocords,there have been no comparable earthquakes with the May 12 Wenchuan earthquake in Chengdu and Longmenshan mountain region.Then,whether the ancient earthquake traces with comparable magnitude in the geological records can be found has become an important scientific issue.The authors and other members of Wenchuan earthquake geological investigation team did fieldwork in the earthquake region for more than one month.Four trenches and one geologic section were excavated along the middle segment of surface faulting of both the central fault and the mountain front fault.And geomorphologic surfaces of deformation were measured.In this paper,we discuss the fact that there is prehistory large earthquake along the seismogenic fault of Wenchuan earthquake from analyzing the accumulated deformation of old and young fault scarps or geomorphologic surfaces,trenching,and comparing the activities of related faults and so on.The result shows that whether at Xiaoyudong,Leigu located on the central fault or Bailu,Hanwang on the mountain front fault,or at other places along the surface faulting of the the Wenchuan earthquake,the height of the fault scarp on the second terrace has a multiple relation with that on the first terrace after the Wenchuan earthquake.The 4 trenches reveal that the dislocation of the marker strata of the second terrace on both sides of fault is twice of that of the Wenchuan earthquake,which shows that there was an earthquake event with the same scale of surface deformation of this MS8.0 Wenchuan earthquake between the formation time of the second terrace in Lomhmenshan area and the May 12 Wenhucan earthquake.Key wrods:MS8.0 Wenchuan Earthquake,Longmenshan Mountains,paleoearthquake,earthquake recurrence
【Fund】: 国家自然科学基金(40841007);; 国家重点基础研究发展计划项目(2004CB418401);; 中国地震局汶川8.0级地震应急科学考察项目共同资助
【CateGory Index】: P315.2
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