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    Volume 45 Issue 1
    Jan.  2020
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    Article Navigation >  Earth Science  > 2020  >  45(1): 303-316
    Wu Xiaoli, Li Rongxi, Hu Jianmin, Liu Futian, Zhao Bangsheng, Qin Xiaoli, 2020. Discovery and Petroleum Geologic Significance of Cenozoic Hydrocarbon Inclusions in Liupanshan Basin, North China. Earth Science, 45(1): 303-316. doi: 10.3799/dqkx.2017.577
    Citation: Wu Xiaoli, Li Rongxi, Hu Jianmin, Liu Futian, Zhao Bangsheng, Qin Xiaoli, 2020. Discovery and Petroleum Geologic Significance of Cenozoic Hydrocarbon Inclusions in Liupanshan Basin, North China. Earth Science, 45(1): 303-316. doi: 10.3799/dqkx.2017.577
    shu

    Discovery and Petroleum Geologic Significance of Cenozoic Hydrocarbon Inclusions in Liupanshan Basin, North China

    doi: 10.3799/dqkx.2017.577
    • 1.

      School of Earth Science and Resources, Chang'an University, Xi'an 710054, China

    • 2.

      Institute of Geomechanics, CAGS, Beijing 100081, China

    • Received Date: 2017-10-07
    • Publish Date: 2020-01-15
      Abstract
    • A large quantity of hydrocarbon inclusions were found in the gypsum of Cenozoic Qingshuiying Formation in Liupanshan basin, which is of a crucial significance to the understanding of the oil and gas reservoir-forming conditions and the development of exploration concept. Development and composition features of hydrocarbon inclusions in gypsum of Qingshuiying Formation were studied by field geological investigation, sample collection and laboratory analysis, etc. Sources and formation of the oil and gas were analyzed by oil-source correlation, and then the conditions and characteristics of petroleum accumulation in Cenozoic of Liupanshan basin were studied. The results show that the oil in the crystal gypsum was derived from the hydrocarbon source rock of Qingshuiying Formation, while the oil in the filament gypsum was derived from the hydrocarbon source rock of Cretaceous Madongshan Formation. The hydrocarbon source rock of Qingshuiying Formation has certain hydrocarbon generating potential, which is the potential source rock in Liupanshan basin. The oil and gas was derived from the Cretaceous hydrocarbon source rock, which can migrate to the upper formation along the fault, and accumulate in Cenozoic. The reservoir traps near the faults connected to the Cretaceous source rock are the favorable oil accumulation zones in Cenozoic.

       

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