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    中国百强科技报刊

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    Volume 44 Issue 6
    Jun.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(6): 2084-2105
    Liu Zilong, Lu Zhanwu, Jia Junlian, Li Wenhui, Ren Yanzong, 2019. Using Deep Seismic Reflection to Profile Deep Structure of Ore Concentrated Area: Current Status and Case Histories. Earth Science, 44(6): 2084-2105. doi: 10.3799/dqkx.2019.020
    Citation: Liu Zilong, Lu Zhanwu, Jia Junlian, Li Wenhui, Ren Yanzong, 2019. Using Deep Seismic Reflection to Profile Deep Structure of Ore Concentrated Area: Current Status and Case Histories. Earth Science, 44(6): 2084-2105. doi: 10.3799/dqkx.2019.020
    shu

    Using Deep Seismic Reflection to Profile Deep Structure of Ore Concentrated Area: Current Status and Case Histories

    doi: 10.3799/dqkx.2019.020
    • 1.

      Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

    • 2.

      Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, China

    • 3.

      Data Processing Center of Geophysical Research Institute, BGP, Zhuozhou 072750, China

    • Received Date: 2018-12-14
    • Publish Date: 2019-06-15
      Abstract
    • Deep seismic reflection profile has been used as the pioneering technology in the study of lithosphere fine structure because of its high detection accuracy and also has played an important role in the structural detection of typical mining areas around the world. In order to study the deep structure and the metallogenic process of the collision orogenic metallogenic system on the Qinghai-Tibet plateau, in this paper, the development status of deep seismic reflection technology is summarized systematically, and the application cases of this technology in typical ore concentration areas in Canada, Australia, China, Russia and Sweden are combed. The influences of deep crust structure on ore-controlling factors in ore centration areas and the relationships between the structure of crust and upper mantle at depth and the deep metallogenic process are illustrated. According to the global examples, the detection results of deep seismic reflection profile provide deep clues for the formation of large ore concentrated areas. The reflective transparent zone may be the upward migration channel of the mantle fluid, forming the mineral and energy sources of ore concentration area, indicating that the mantle material is involved in mineralization. Fracture systems characterized by strong reflectivity, including large-scale faults, detachments and crustal shear zones, are pathways through which metallogenic fluids migrate upward from the lower crust. The"bright spot"in the deep seismic reflection profiles of ore concentrated areas may be the reflection of the residual magma chamber formed after the deep magma of volcanic activity surges into the middle crust. Revealing the deep fine structure not only plays an important role in the reconstruction of the tectonic historical evolution of ore concentration area, but also has crucial guiding significance for the determination of the future metallogenic potential and the target area of the foreground.

       

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