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    Volume 39 Issue 10
    Oct.  2014
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    Article Contents
    Zhao Yanjun, Liu Chenglin, Zhang Hua, Wang Licheng, Feng Yong, Wu You, Liu Baokun, 2014. Characteristics and Geological Significance of Fluid Inclusions in Halite of the First Member of Shahejie Formation in Shulu Depression, Bohai Bay Basin. Earth Science, 39(10): 1355-1363. doi: 10.3799/dqkx.2014.127
    Citation: Zhao Yanjun, Liu Chenglin, Zhang Hua, Wang Licheng, Feng Yong, Wu You, Liu Baokun, 2014. Characteristics and Geological Significance of Fluid Inclusions in Halite of the First Member of Shahejie Formation in Shulu Depression, Bohai Bay Basin. Earth Science, 39(10): 1355-1363. doi: 10.3799/dqkx.2014.127

    Characteristics and Geological Significance of Fluid Inclusions in Halite of the First Member of Shahejie Formation in Shulu Depression, Bohai Bay Basin

    doi: 10.3799/dqkx.2014.127
    • Received Date: 2014-02-23
    • Publish Date: 2014-10-01
    • A large amount of primary single-phase aqueous fluid inclusions and secondary petroleum inclusions are discovered in the halite in the first member of Palaeogene Shahejie Formation in Shulu depression, which facilitates the determination of the origin of evaporite and the migration and preservation conditions of oil and gas. In this paper, the formation time and the trapping paleopressure of fluid inclusions and the burial history of oil and gas are analyzed by linking the homogenization temperature of both the primary single-phase aqueous fluid inclusions and secondary petroleum inclusions with the petrography of halite. As the results, the homogenization temperature of the aqueous inclusion, which is symbiosis with the petroleum inclusions, ranges from 66.5 to 91.5 ℃ and 103.7 to 108.9 ℃, respectively. The trapping time of the former is about 10.56 to 10.11 Ma and the trapping time of the latter is about 1.10 Ma. It is concluded that the time of oil and gas fluid entering into the salt rock is about the middle-late Guantao Formation and Pleistocene, which is also evidenced by the investigation of the oil and gas generation history. The paleopressure coefficient of the middle part of the salt rock modeled by fluid inclusions is up to 1.64, suggesting that there existed a hyperpressure system under the salt rock which probably facilitated the migration and preservation of oil and gas.

       

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