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引用本文:雷东宁,蔡永建,乔岳强,余松,吴建超,缪卫东.???-????????жι???????????????????[J].大地测量与地球动力学,2012,32(5):41-47.
作者姓名:雷东宁  蔡永建  乔岳强  余松  吴建超  缪卫东
作者单位:1. 中国地震局地震研究所(地震预警湖北省重点实验室),武汉430071;武汉地震工程研究院,武汉430071
2. 中国地震局地震研究所(地震预警湖北省重点实验室),武汉430071;武汉地震工程研究院,武汉430071;中国地质大学(武汉)地球科学学院,武汉430074
基金项目:中国地震局地震研究所所长基金(IS200856069)
摘    要:????????ò?????????????????????????????,?????????????жι?????Ρ??????????????????????????????????????????,?????????;????????????????????????????????????????0.64~0.85 mma -1;???????????????,??????????????????????;??????????????С?????????????????????,????????????????й???????????

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STUDY ON TECTONIC DEFORMATION AND QUATENARY ACTIVITY OF MIDDLE SEGMENT OF BAIHE-GUCHENG FAULT BELT
Lei Dongning,Cai Yongjian,Qiao Yueqiang,Yu Song,Wu Jianchao,and Miao Weidong.STUDY ON TECTONIC DEFORMATION AND QUATENARY ACTIVITY OF MIDDLE SEGMENT OF BAIHE-GUCHENG FAULT BELT[J].Journal of Geodesy and Geodynamics,2012,32(5):41-47.
Authors:Lei Dongning  Cai Yongjian  Qiao Yueqiang  Yu Song  Wu Jianchao  and Miao Weidong
Institution:1,2) 1) Hubei Key Laboratory of Earthquake Early Warning,Institute of Seismology,CEA,Wuhan 4300712) Institute of Earthquake Engineering of Wuhan 4300713) Faculty of Earth Science,China University of Geosciences,Wuhan 430074
Abstract:Through field survey, with geological and geomorpohologic methods and dating the fault gouge and Quaternary sediments, we made certain study on tectonic deformation and activity of the middle segment of Baihe Gucheng fault. Some conclusions can be drawn that the fault belt suffered from multi stage tectonic deformation and it is clearly zoning. The lifting velocity of fault and its neighbouring area ranges from 0.64 mma -1 to 0.85 mma-1 since the Middle stage of Late Pleistocene. The fault was predominantly active in the Early Quaternary with sinistral slip component. The seismicity of fault and nearby tends to enhance in time domain and is tectonically relatated to the fault in spatial domain.
Keywords:Baihe-Gucheng fault belt  tectonic deformation  Quaternary activity  lifting-velocity  left lateral slip
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