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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 Contents
    Article Navigation >  Earth Science  > 2014  >  39(8): 1079-1098
    Xu Yadong, Liang Yinping, Jiang Shangsong, Luo Mansheng, Ji Junliang, Zhang Zongyan, Wei Yi, Song Bowen, 2014. Evolution of Cenozoic Sedimentary Basins in Eastern China. Earth Science, 39(8): 1079-1098. doi: 10.3799/dqkx.2014.096
    Citation: Xu Yadong, Liang Yinping, Jiang Shangsong, Luo Mansheng, Ji Junliang, Zhang Zongyan, Wei Yi, Song Bowen, 2014. Evolution of Cenozoic Sedimentary Basins in Eastern China. Earth Science, 39(8): 1079-1098. doi: 10.3799/dqkx.2014.096
    shu

    Evolution of Cenozoic Sedimentary Basins in Eastern China

    doi: 10.3799/dqkx.2014.096
    • 1.

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

    • 2.

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

    • 3.

      Material Geological Data Center, Ministry of Land and Resources, Sanhe 065201, China

    • 4.

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

    • 5.

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

    • Received Date: 2014-03-25
    • Publish Date: 2014-08-01
      Abstract
    • With subduction collision between Eurasian plate and surrounding plates such as Indian, Australian, Philippine and Pacific plates, a series of marginal sea basins, and faulted-downwarped basins formed in the continental margin of eastern China, mainly including Songliao, Bohai Bay, Jianghan, Subei, East China Sea, Pearl River Mouth and Beibuwan basins. Based on Mesozoic tectonic background analysis and Cenozoic distribution characteristics of sedimentary basins in eastern China, sedimentary sequence and tectonic evolution of 7 main basins are analyzed in detail.through a comparative study of tectonic evolution of the surrounding plates and the Tan-Lu fault, volcanism, low temperature thermochronology, climatic evolvement, and so on.It is found that the tectonic evolution of the sedimentary basins in eastern China can be divided into three phases, which are Paleocene-Eocene, Oligocene-Early Miocene and Late Miocene-Quaternary respectively.

       

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