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汶川M_S8.0地震对龙门山断裂带附近地应力环境影响初探——以北川、江油地区为例
引用本文:丰成君,陈群策,谭成轩,吴满路,秦向辉,廖椿庭.汶川M_S8.0地震对龙门山断裂带附近地应力环境影响初探——以北川、江油地区为例[J].地震学报,2013,35(2):137-150.
作者姓名:丰成君  陈群策  谭成轩  吴满路  秦向辉  廖椿庭
作者单位:1.中国北京 100081 中国地质科学院地质力学研究所
基金项目:国土资源部深部探测技术与实验研究专项,中国地质调查局项目"青藏高原东缘主要断裂带地应力监测"
摘    要:为探讨汶川MS8.0地震对龙门山断裂带现今地应力环境的影响,2009年10—12月,在龙门山断裂带的北川、江油地区开展了3个200m深度钻孔水压致裂地应力测量,获得了汶川MS8.0地震发生1年多以后断裂带附近地壳浅表层地应力环境.根据研究区内的原地应力测量结果及汶川MS8.0地震引起的断层错动等资料,运用线弹性有限元数值模拟方法,计算得到了由断层错动位移所产生的附加应力,并推算了ZK02和ZK03位置震前应力分布特征.通过对比分析,揭示了断裂带附近地应力场的变化规律,探讨了汶川MS8.0地震对龙门山断裂带附近地应力环境的影响.

关 键 词:龙门山断裂带    水压致裂地应力测量    地应力环境    线弹性有限元数值模拟
收稿时间:2011-12-23

A preliminary study of the influence of Wenchuan MS8.0 earthquake on in-situ stress state near Longmenshan fault zone: A case study in Beichuan and Jiangyou areas
Feng Chengjun , Chen Qunce , Tan Chengxuan , Wu Manlu , Qin Xianghui , Liao Chunting.A preliminary study of the influence of Wenchuan MS8.0 earthquake on in-situ stress state near Longmenshan fault zone: A case study in Beichuan and Jiangyou areas[J].Acta Seismologica Sinica,2013,35(2):137-150.
Authors:Feng Chengjun  Chen Qunce  Tan Chengxuan  Wu Manlu  Qin Xianghui  Liao Chunting
Affiliation:1.Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China2.Key Laboratory of Neotectonic Movement & Geohazard, Ministry of Land and Resources, Beijing 100081, China
Abstract:In order to investigate the influence of Wenchuan MS8.0 earthquake on in-situ stress state near the Longmenshan fault zone, hydraulic fracturing measurements in three 200 m-deep boreholes were carried out in Beichuan and Jiangyou areas near the fault zone from Oct. to Dec., 2009, and the distribution of current in-situ stress there at the time more than 1 year after the earthquake was analyzed. Based on the in-situ stress measurements and coseismic fault displacement in the study areas, the distribution of additional stress induced by fault motion was calculated with a linear-elastic finite element simulation, and then distribution of the principal stress at the two boreholes before the earthquake was calculated. Finally, the influence of Wenchuan MS8.0 earthquake on in-situ stress state in a superficial zone near Longmenshan fault was discussed through comparative analysis. 
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