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    Volume 37 Issue 6
    Jun.  2012
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    Article Navigation >  Earth Science  > 2012  >  37(6): 1243-1251
    ZHANG Xu, ZHANG Da, TAN Han-dong, LIN Quan-sheng, DI Yong-jun, LV Liang-ji, LIU Min, WANG Gai-mei, 2012. Geological and Geophysical Model of Thrust Controlling on Iron Ore Deposits in the Southwestern Fujian Province. Earth Science, 37(6): 1243-1251. doi: 10.3799/dqkx.2012.132
    Citation: ZHANG Xu, ZHANG Da, TAN Han-dong, LIN Quan-sheng, DI Yong-jun, LV Liang-ji, LIU Min, WANG Gai-mei, 2012. Geological and Geophysical Model of Thrust Controlling on Iron Ore Deposits in the Southwestern Fujian Province. Earth Science, 37(6): 1243-1251. doi: 10.3799/dqkx.2012.132
    shu

    Geological and Geophysical Model of Thrust Controlling on Iron Ore Deposits in the Southwestern Fujian Province

    doi: 10.3799/dqkx.2012.132
    • 1.

      State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

    • 2.

      Key Laboratory of Lithospheric Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing 100083, China

    • Received Date: 2012-07-19
      Available Online: 2021-11-09
    • Publish Date: 2012-06-15
      Abstract
    • The southwestern Fujian is located in southwestern Wuyishan mineralization zone, where nappe (slippage) structures extensively developed after a multi-stage tectonic evolution since the Proterozoic, with control over "Ma Keng"-small, medium and large iron polymetallic deposits in the region. It is found in this study on nappe structures associated with ore-bearing rocks and nappe interfaces that the ore-bearing strata mainly consist of C2+3-P1q; the nappe mainly occurred along the AnD/C1l and C1l/C2+3+P1q interfaces; and these two regional nappe structures may be the geochemical shield of the hydrothermal ore-forming fluid. A ore-controlling geological-geophysical model of the nappe structure in southwestern Fujian is established by surface geological analysis of distribution and tectonic framework of the deep ore-bearing rock and nappe interface combining the interpretation of deep controlled source audio magnetotelluric method (CSAMT), which will certainly facilitate deep prospecting.

       

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