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    Volume 39 Issue 8
    Aug.  2014
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    Article Navigation >  Earth Science  > 2014  >  39(8): 1140-1154
    Tang Tingting, He Weihong, Wang Chenggang, Ji Xingxing, Hao Yiwei, Zou Yarui, 2014. Evolution of Mesozoic Sedimentary Basins in Wuyi-Yunkai Area. Earth Science, 39(8): 1140-1154. doi: 10.3799/dqkx.2014.100
    Citation: Tang Tingting, He Weihong, Wang Chenggang, Ji Xingxing, Hao Yiwei, Zou Yarui, 2014. Evolution of Mesozoic Sedimentary Basins in Wuyi-Yunkai Area. Earth Science, 39(8): 1140-1154. doi: 10.3799/dqkx.2014.100
    shu

    Evolution of Mesozoic Sedimentary Basins in Wuyi-Yunkai Area

    doi: 10.3799/dqkx.2014.100
    • 1.

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

    • 2.

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

    • 3.

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

    • 4.

      Wuhan Institute of Geology and Mineral Resources, Wuhan 430223, China

    • Received Date: 2014-03-20
    • Publish Date: 2014-08-01
      Abstract
    • In order to study the sendimentary basin evolution of the Wuyi-Yunkai area, in this paper the area is divided into 5 stratigraphic regions. Based on the previous studies on the lithostritagraphy combinations, fossil assemblages, isotopic geochronology and tectonics of this area, types of sedimentary basin in the Wuyi-Yunkai area are identified, and their formation and evolution are investigated. The evolutional history of the sedimentary and tectonic features of the study area shows that the basin and structure have experienced three major evolutionary stages in Mesozoic. In the Early-Middle Triassic, the research area entered the marine-continental alternating epicontinental sea stage because of transgressions with the crust uplifting, the main sea level dropping and the sea gradually receding to the west or southwest. In the Middle Jurassic-Cretaceous, a series of subduction-accretionary complex belt formed in Taiwan, and inland areas were bounded by the Zhenghe-Dapu fracture, with fault basin (including volcanoes) developed in the west and its east entering evolutionary stage of intra-arc graben basin whose late stage was fault basin evolution, mainly influenced by the low subduction of the Pacific plate.

       

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