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    Volume 44 Issue 7
    Jul.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(7): 2551-2566
    Yang Wenpeng, Zhang Lidong, Zhang Jianfeng, Jiang Haiyang, Lü Shijia, Li Xinpeng, Wan Taiping, 2019. Deformation Characteristics and Genesis of the Xinkailing-Keluo Complex in NE China. Earth Science, 44(7): 2551-2566. doi: 10.3799/dqkx.2018.570
    Citation: Yang Wenpeng, Zhang Lidong, Zhang Jianfeng, Jiang Haiyang, Lü Shijia, Li Xinpeng, Wan Taiping, 2019. Deformation Characteristics and Genesis of the Xinkailing-Keluo Complex in NE China. Earth Science, 44(7): 2551-2566. doi: 10.3799/dqkx.2018.570
    shu

    Deformation Characteristics and Genesis of the Xinkailing-Keluo Complex in NE China

    doi: 10.3799/dqkx.2018.570

    • Geological Survey Institute of Heilongjiang, Harbin 150036, China

    • Received Date: 2017-11-16
    • Publish Date: 2019-07-15
      Abstract
    • Xinkailing-Keluo complex, located in Nenjiang-Heihe tectonic belt, NE China, has fully undergone regional tectonic movement and therefore recorded plentiful evolution information. Its residual deformation signatures and genetic mechanisms could provide key clues about regional tectonic evolution history of not only the adjacent region but also the whole north-east area of China. Based on detailed field survey, this paper conducted systematic studies on different types of structure units, foliation of mylonite rock, stretching lineation of minerals, A-type fold, asymmetrical fold, augen-shaped rotational structure and microscopic book skew structure.The results revealed a significant fact two wings of the complex have the extension of NW and SE respectively, The mineral of zircon have been identified from internal biotite-plagioclase gneiss and intrusive dioritic-porphyrite body in mylonite country rock.Its U-Pb dating of zircon and regional study both indicated these deformation mainly occurred during Middle-Jurasic (167 Ma), and reached metamorphic peak during 170-163 Ma.Then it was uplifted by tectonic movement and exposed to the ground in late Middle-Jurasic. Xinkailing-Keluo complex was composed of three layers architecture, the upper cap rock, middle zone and lower complex.The internal part is mainly composed by granite, which are much younger than its outer part.The metamorphic temperature ranged from 400 to 500 degree, reaching extent of greenschist facies and was followed by retrograde metamorphism. Later, the regional uplift happened due to the granite magma underplating and the Xinkailing-Keluo magmatic core complex formed under regional stretch tectonic background.

       

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