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    Volume 43 Issue 11
    Nov.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(11): 4180-4192
    Wang Deliang, Mei Lianfu, Liu Yunsheng, Wu Lulu, Min Caizheng, Luo Jin, 2018. Mesozoic-Cenozoic Episodic Subsidence and Migration of Jianghan Basin in Extensional Composite Basin-Mountain System. Earth Science, 43(11): 4180-4192. doi: 10.3799/dqkx.2018.211
    Citation: Wang Deliang, Mei Lianfu, Liu Yunsheng, Wu Lulu, Min Caizheng, Luo Jin, 2018. Mesozoic-Cenozoic Episodic Subsidence and Migration of Jianghan Basin in Extensional Composite Basin-Mountain System. Earth Science, 43(11): 4180-4192. doi: 10.3799/dqkx.2018.211
    shu

    Mesozoic-Cenozoic Episodic Subsidence and Migration of Jianghan Basin in Extensional Composite Basin-Mountain System

    doi: 10.3799/dqkx.2018.211
    • 1.

      Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China

    • 2.

      Research Institute of Exploration and Development of Jianghan Oilfield, SINOPEC, Wuhan 430000, China

    • 3.

      Research Institute of China National Offshore Oil Company Ltd., Beijing 100027, China

    • Received Date: 2018-05-10
    • Publish Date: 2018-11-15
      Abstract
    • An extensional composite basin-mountain system is formed by Jianghan basin and its peripheral mountains, and there might be coupling relationship between the basin and orogenic belt. In this study, the subsidence history analysis shows the feature of episodic subsidence in Jianghan basin, which is divided into three rifting stages:Episodic Ⅰ Late Cretaceous, Episodic Ⅱ Paleocene Shashi-Early Eocene Xingouzui phase and Episodic Ⅲ Early Eocene Jingsha-Oligocene Jinghezhen phase. The subsidence center migrated regularly, and it moved to Jiangling depression in the Episodic Ⅱ and Qianjiang depression in the Episodic Ⅲ. The regular migration of subsidence center in the extensional composite basin-mountain system might be affected by many factors. In the meantime, it displays the response relationship between the migration of subsidence center and the peripheral mountains. The east mountains (Dabie orogen, Mufushan massif and Edong fold-thrust belt) uplift as the subsidence center migrates westward. And west mountains (Huangling massif and Xiang'exi fold-thrust belt) uplift as the subsidence center migrates eastward. In addition, the subsidence center shows the character of "deviation type" which migrates farther away from where the orogen uplifts. Meanwhile, the migration of subsidence center may also be affected by the changes of mantle diapir.

       

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