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The M_S 4.1 Reservoir-induced Hujiaping Earthquake in the Yangtze Three Gorges Reservoir Region
Authors:Che Yongtai  Chen Junhu  Zhang Lifen  Yu Jinzi  Liu Chenglong and Zhang Weihua
Institution:[1]Institute of Geology, China Earthquake Administration, Beijing 100029, China [2]Earthquake Administration of Hubei Province,Wuhan 430071 ,China
Abstract:In this paper,based on the collected data and earthquake field investigation,characteristics of the MS4.1 Hujiaping earthquake of November 22,2008 at Guizhou town in Zigui county,Hubei Province and the geological and hydrogeological conditions and seismicity background of the area are analyzed,and the earthquake disaster is presented. Some scientific issues relating to earthquake precursors and the cause of the earthquake is discussed. The authors consider that the earthquake is a tectonic type reservoir-induced earthquake,occurring along the Xiannvshan fault under the joint action of reservoir water loading and water infiltration,and that there were certain suspected anomalies appearing in the gravity field before the earthquake. The cause of the earthquake may also be related to the effect of the Wenchuan earthquake on the local stress field.
Keywords:Yangtze Three Gorges    Xiannvshan fault    Reservoir-induced earthquake    The MS4  1 Hujiaping earthquake
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