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    中国百强科技报刊

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    Volume 39 Issue 8
    Aug.  2014
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    Article Navigation >  Earth Science  > 2014  >  39(8): 929-953
    He Weihong, Tang Tingting, Yue Mingliang, Deng Jinfu, Pan Guitang, Xing Guangfu, Luo Mansheng, Xu Yadong, Wei Yi, Zhang Zongyan, Xiao Yifan, Zhang Kexin, 2014. Sedimentary and Tectonic Evolution of Nanhuan-Permian in South China. Earth Science, 39(8): 929-953. doi: 10.3799/dqkx.2014.087
    Citation: He Weihong, Tang Tingting, Yue Mingliang, Deng Jinfu, Pan Guitang, Xing Guangfu, Luo Mansheng, Xu Yadong, Wei Yi, Zhang Zongyan, Xiao Yifan, Zhang Kexin, 2014. Sedimentary and Tectonic Evolution of Nanhuan-Permian in South China. Earth Science, 39(8): 929-953. doi: 10.3799/dqkx.2014.087
    shu

    Sedimentary and Tectonic Evolution of Nanhuan-Permian in South China

    doi: 10.3799/dqkx.2014.087
    • 1.

      State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

    • 2.

      Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China

    • 3.

      Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

    • 4.

      State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

    • 5.

      Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, China

    • 6.

      Nanjing Institute of Geology and Mineral Resources, Nanjing 210016, China

    • Received Date: 2014-03-28
    • Publish Date: 2014-08-01
      Abstract
    • This paper firstly analyzes the lithological features, the thickness of sequence, metamorphical features and the sedimentary environment of seven Nanhuan-Permian combined sections from South China, then analyzes the petrological assemblages including ophiolites, basalts, island arc igneous and the TTG-GG suites (granites) from the area of south margin of Yangtze continental block and the area of Cathay accreting block and lastly analyzes the basin features based on the lithology of each unit (formation) from South China. Based on the above-mentioned analyses, four stages of tectonic evolution of South China are identified and it is concluded that the collision between the Yangtze continental block and Cathay accreting block occurred at the end of the Early Paleozoic along the northeastern part and the collision along the southwestern part occurred at the end of the Permian.

       

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