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《Progress in Geophysics》 2013-03
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Faults activity and stress state in the northeast segment of Longmenshan faults zone

DU Jian-jun1,2,CHEN Qun-ce2,MA Yin-sheng2,AN Qi-mei3, WU Man-lu2,MENG Wen2,LI Guo-qi2(1.Key Laboratory of Neotectonic Movement and Geohazard,Ministry of Land and Resources,Beijing 100081,China; 2.Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,China; 3.Institute of Crustal Dynamics,China Earthquake Administration,Beijing 100085,China)  
After Wenchuan MS 8.0 earthquake,the problem people concerned is seismic active trend in Longmenshan area.Based on structure characteristics and some data of hydraulic fracturing stress measurement of more than 15 boreholes,authors analyze the relationship of stress state and fault activity,to study the risk of another strong earthquake or strong aftershocks in the northeast segment of Longmenshan fault zone.The results show that the stress state is helpful to thrust fault and strike-slip fault movement in study area.The activity of different faults is quite uniform with stress state.The stress and strain energy is accumulating although the faults activity of study area are in atresic state in the northeast segment of Longmenshan fault zone.The long-term energy accumulation caused Wenchuan 8.0 earthquake.The energy of Wenchuan earthquake and its aftershocks transfer and accumulate towards the northeast segment of Longmenshan fault zone.The result is that the risk of strong earthquake is still high in the northeast segment of Longmenshan fault zone.
【Fund】: 国家深部探测技术与实验研究专项(SinoProbe-06-03);; 中国地质调查局地质大调查项目(项目编号:1212011120102)联合资助
【CateGory Index】: P315
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