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    Volume 45 Issue 5
    May  2020
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    Article Navigation >  Earth Science  > 2020  >  45(5): 1636-1652
    Hu Jun, Yu Xinqi, Lu Zongyue, Zeng Yan, Liu Xiu, Wang Zhaofan, 2020. Ductile-Compressional Deformation of Kanggur Ductile Deformation Zone in the Eastern Tianshan Mountains: A Case Study of Huangshandong Area of Hami City. Earth Science, 45(5): 1636-1652. doi: 10.3799/dqkx.2019.195
    Citation: Hu Jun, Yu Xinqi, Lu Zongyue, Zeng Yan, Liu Xiu, Wang Zhaofan, 2020. Ductile-Compressional Deformation of Kanggur Ductile Deformation Zone in the Eastern Tianshan Mountains: A Case Study of Huangshandong Area of Hami City. Earth Science, 45(5): 1636-1652. doi: 10.3799/dqkx.2019.195
    shu

    Ductile-Compressional Deformation of Kanggur Ductile Deformation Zone in the Eastern Tianshan Mountains: A Case Study of Huangshandong Area of Hami City

    doi: 10.3799/dqkx.2019.195
    • 1.

      School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

    • 2.

      Geophysical Survey Center of China Geological Survey, Langfang 065000, China

    • 3.

      Marine Geological Survey Center, Haikou 571127, China

    • Received Date: 2019-08-06
    • Publish Date: 2020-05-15
      Abstract
    • A east-west trending ductile deformation zone was identified between the Kanggur fault and Yamansu fault within the Carboniferous sedimental-volcanic series in the eastern Tianshan mountains. The deformation zone exhibits different characteristics in its evolutionary process, namely, the early stage ductile compressional deformation, and the later right lateral shear deformation. In this paper, the macrostructure (foliation, lineation, symmetrical boudinage structure and asymmetric fold, etc.), and microstructure (pressure shadow, boudinage structure, dynamic recrystallization, different types of gravel deformation, etc.) of early ductile compressed deformation were studied in detail. Systematic measurement of the finite strains of quartz and triaxial strain rate in mylonites indicates that the strain type in general compression is L-S and LS tectonites. The quartz grains occur as subgrain rotation recrystallization and a small amount of grain boundary migration recrystallization, and the feldspar porphyroclasts are elongated and some are fully bulging recrystallized. Quartz C-axis fabrics (EBSD) reveal that quartz fabrics are mainly middle temperature prismatic slip and rhomb slip system, and the later superimposed low temperature is slip-based. It is suggested that the deformation temperature of the early ductile compressional ranges from 450 ℃ to 550 ℃. Combined with regional tectonic, the early ductile compressional of Kanggur ductile deformation zone was formed in 300-290 Ma, which was related to the intracon-tinental N-S compression environment after collision between the Tarim plate and the middle Tianshan plate.

       

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