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    Volume 42 Issue 12
    Dec.  2017
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    Article Navigation >  Earth Science  > 2017  >  42(12): 2193-2207
    Chang Ruihong, Li Weimin, Liu Yongjiang, Liang Chenyue, Li Jing, Zhang Li, Liu Xinyue, Fan Wenliang, 2017. Structural Properties and Kinematic Analysis of Lianshanguan Ductile Shear Zone in Northern Liao-Ji Rift Zone, Northeastern North China Craton. Earth Science, 42(12): 2193-2207. doi: 10.3799/dqkx.2017.140
    Citation: Chang Ruihong, Li Weimin, Liu Yongjiang, Liang Chenyue, Li Jing, Zhang Li, Liu Xinyue, Fan Wenliang, 2017. Structural Properties and Kinematic Analysis of Lianshanguan Ductile Shear Zone in Northern Liao-Ji Rift Zone, Northeastern North China Craton. Earth Science, 42(12): 2193-2207. doi: 10.3799/dqkx.2017.140
    shu

    Structural Properties and Kinematic Analysis of Lianshanguan Ductile Shear Zone in Northern Liao-Ji Rift Zone, Northeastern North China Craton

    doi: 10.3799/dqkx.2017.140
    • 1.

      College of Earth Sciences, Jilin University, Changchun 130061, China

    • 2.

      Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Land and Resources, Changchun 130061, China

    • 3.

      Key laboratory for Evolution of Past Life and Environment in Northeast Asia, Ministry of Education, Changchun 130026, China

    • 4.

      Changchun Gold Research Institute, Changchun 130012, China

    • 5.

      Shenyang Geological Survey Center, China Geological Survey, Shenyang 110034, China

    • Received Date: 2017-03-08
    • Publish Date: 2017-12-15
      Abstract
    • The ductile shear zone is widely discovered in the lithospheric crust, and it contains abundance environmental parameters such as stress, strain temperature and pressure, hence it is an important object for the study of structural analysis, rheology and genetic mechanism. The Liao-Ji rift zone is one of the ancient primitive activities of the North China craton, located in the east of Liaoning Province and North of Jilin Province. The Lianshanguan granitic body, exposed in the Northern margin of Liao-Ji rift zone, experienced complex metamorphic deformation. The mylonitic in the ductile shear zone have obvious dextral strike-slip characteristics with an NWW strike. The observation and analysis of the microstructure of mylonitic reveals that the taconite developed in shear zone is S-SL type, representing a flattening strain. Kinematics vorticity of 0.91-0.97, which are greater than 0.75, indicates that the shearing is formed in the general shear dominated simple shear. In addition, The quartz dynamic recrystallization is obvious, while the mica shows plastic elongation. The quartz c-axis EBSD analysis shows that the quartz fabric is characterized by the middle to low temperature rhomb slip system, corresponding deformation temperature of 450-550℃, consistent with a greenschist-low amphibolite facies condition. Based on the previous studies, the forming age of the ductile shear deformation is considered to be the late Early Proterozoic. In conclusion, the Lianshanguan granitic body suffered an initial uplift stage, resulting extension-stretching-decollement within the Liaohe Formation surrounding the granitic body. Subsequently, the studied area was suffered a S-N directing compression, and led to the dextral strike-slip ductile shearing.

       

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