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    Volume 42 Issue 1
    Jan.  2017
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    Article Navigation >  Earth Science  > 2017  >  42(1): 130-141
    Tian Dongmei, Jiang Tao, Zhang Daojun, Zuo Qianmei, Sun Hui, He Xiaohu, 2017. Genesis Mechanism and Characteristics of Submarine Channel: A Case Study of the First Member of Yinggehai Formation in Ledong Area of Yinggehai Basin. Earth Science, 42(1): 130-141. doi: 10.3799/dqkx.2017.010
    Citation: Tian Dongmei, Jiang Tao, Zhang Daojun, Zuo Qianmei, Sun Hui, He Xiaohu, 2017. Genesis Mechanism and Characteristics of Submarine Channel: A Case Study of the First Member of Yinggehai Formation in Ledong Area of Yinggehai Basin. Earth Science, 42(1): 130-141. doi: 10.3799/dqkx.2017.010
    shu

    Genesis Mechanism and Characteristics of Submarine Channel: A Case Study of the First Member of Yinggehai Formation in Ledong Area of Yinggehai Basin

    doi: 10.3799/dqkx.2017.010
    • 1.

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

    • 2.

      Zhanjiang Branch of CNOOC Ltd., Zhanjiang 524057, China

    • Received Date: 2016-06-10
    • Publish Date: 2017-01-15
      Abstract
    • The submarine channel is one of the important targets for deep water hydrocarbon exploration as well as the key point for the investigation into source and sink. Based on the newly acquired 3D seismic data and 3 boreholes in the Ledong area of the Yinggehai basin, the sequence stratigraphic framework for the first member of the Yinggehai Formation is set up. The development of every fourth-order sequence is derived by the enough sediment supply and high frequency sea-level changes under stable tectonic setting. The submarine channels occur in lowstand systems of every fourth-order sequence, which can be classified into slope channel and axial channel. Furthermore, the evolution of submarine channels is described, such as flowing through the lower topography with a convergent system, being reworked by mass-transport deposits (MTDs) and diapirs. Controlled by the sediment supply, high-frequency sea-level fluctuation and regional tectonic activities, the number and scale of submarine channels gradually decrease. The recorded high-frequency sea-level fluctuation by high sedimentary rate in Ledong area makes it possible to better understand the evolution and controlling factors of submarine channels, which facilitates future hydrocarbon exploration.

       

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