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    LIU Wei-liang, YANG Zhen-fa, GU Man, WU De-chao, WANG Dao-yong. The Fubian River fault activity near the Jinchuan hydropower station, Dadu River, Sichuan[J]. Sedimentary Geology and Tethyan Geology, 2007, 27(4): 74-79.
    Citation: LIU Wei-liang, YANG Zhen-fa, GU Man, WU De-chao, WANG Dao-yong. The Fubian River fault activity near the Jinchuan hydropower station, Dadu River, Sichuan[J]. Sedimentary Geology and Tethyan Geology, 2007, 27(4): 74-79.
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    The Fubian River fault activity near the Jinchuan hydropower station, Dadu River, Sichuan

    • 1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, Guangdong, China;

    • 2. GraduateSchool, Chinese Academy of Sciences, Beijing 100049, China;

    • 3. North China University of Water Conservancy and Electric Power, Zhengzhou 450011, Henan, China;

    • 4. Chengdu University of Technology, Chengdu 610059, Sichuan, China

    More Information
    • Received Date: June 29, 2006
    • Revised Date: November 03, 2006
    • Published Date: December 29, 2007
      Graphical Abstract
      • Abstract
    • It is only a 35-km distance from the Fubian River fault to the large-scale Jinchuan hydropower station, Dadu River, Sichuan. Thus the currently intense seismic activities should be considered as important factors in the evaluation of the stability of the hydropower station. The evidence and activity of the fault are examined on the basis of geophysics, seismology, geology and geomorphology. The fault has been found, for the first time, to dissect the Quaternary strata, however it has no harm to the safety of the hydropower station.
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