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    中国百强科技报刊

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    Volume 46 Issue 11
    Nov.  2021
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    Article Contents
    Qin Ya, Feng Zuohai, Huang Jingzhe, Bai Yuming, Wu Jie, Zhang Guilin, Wan Lei, 2021. Discovery of Sanmen Ductile Shear Zone in North Guangxi and Its Tectonic Significances. Earth Science, 46(11): 4017-4032. doi: 10.3799/dqkx.2020.353
    Citation: Qin Ya, Feng Zuohai, Huang Jingzhe, Bai Yuming, Wu Jie, Zhang Guilin, Wan Lei, 2021. Discovery of Sanmen Ductile Shear Zone in North Guangxi and Its Tectonic Significances. Earth Science, 46(11): 4017-4032. doi: 10.3799/dqkx.2020.353

    Discovery of Sanmen Ductile Shear Zone in North Guangxi and Its Tectonic Significances

    doi: 10.3799/dqkx.2020.353
    • Received Date: 2020-11-05
      Available Online: 2021-12-04
    • Publish Date: 2021-11-30
    • Based on the field geological investigation, microstructural observation and magnetic fabric of tectonites, it recognized a large ductile shear zone in Sanmen area of North Guangxi, also defined the deformation age of Sanmen ductile shear zone by hydrothermal zircon U-Pb dating. The ductile shear zone has typical macroscopic and microstructural characteristics of mylonite series, such as penetrating schistosity, rotational porphyroclast systems, stretching lineation, eyeball structures, domino structures, A-type fold, wavy extinction, deformation twins, core and mantle textures and S-C fabric. Anisotropy of magnetic susceptibility (P values) shows Sanmen ductile shear zone trending in NNE and inclination of NWW. Kinematics orientation research shows that the Sanmen ductile shear zone has left-lateral thrust shear in the early stage and right-lateral normal slip shear in the late stage, magnetic susceptibility ellipsoid (E values) indicates that the rock deformation in Sanmen ductile shear zone is mainly flattened strain, suggesting that its kinematic direction is mainly left-lateral thrust shear. The hydrothermal zircon U-Pb dating result of mafic mylonite is 441±2 Ma, which represents the deformation age of Sanmen ductile shear zone. Based on the study of magnetic fabric, kinematics and tectonic chronology of Sanmen ductile shear zone, combined with regional geological data, it is considered that Sanmen ductile shear zone is the product of the recoil of the Caledonian Cathaysian block in South China from SE to NW to the Yangtze block. The discovery of the Sanmen ductile shear zone reveals the way and age of collision of Yangtze and Cathaysian blocks, and deepens the understanding of Caledonian tectonic evolution of the South China.

       

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