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    Volume 48 Issue 2
    Feb.  2023
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    Article Navigation >  Earth Science  > 2023  >  48(2): 776-792
    Shi Xiaofan, Luo Jinglan, Chen Lin, Fu Yong, Xu Shouli, Yan Min, Liu Fang, 2023. Hydrocarbon Charging Stages and Their Differences in Different Structural Units of the Deep Zhuhai Formation in Wenchang A Sag, Pearl River Mouth Basin. Earth Science, 48(2): 776-792. doi: 10.3799/dqkx.2022.458
    Citation: Shi Xiaofan, Luo Jinglan, Chen Lin, Fu Yong, Xu Shouli, Yan Min, Liu Fang, 2023. Hydrocarbon Charging Stages and Their Differences in Different Structural Units of the Deep Zhuhai Formation in Wenchang A Sag, Pearl River Mouth Basin. Earth Science, 48(2): 776-792. doi: 10.3799/dqkx.2022.458
    shu

    Hydrocarbon Charging Stages and Their Differences in Different Structural Units of the Deep Zhuhai Formation in Wenchang A Sag, Pearl River Mouth Basin

    doi: 10.3799/dqkx.2022.458
    • 1.

      State Key Laboratory of Continental Dynamics, Northwestern University, Xi'an 710069, China

    • 2.

      Zhanjiang Branch of CNOOC Ltd., Zhanjiang 524057, China

    • Received Date: 2022-12-04
    • Publish Date: 2023-02-25
      Abstract
    • The Paleogene Zhuhai Formation in the deep Wenchang A Sag of the Pearl River Mouth Basin is rich in oil and gas resources, but the distribution of oil and gas reservoirs in different regions is complex, and the study of inclusions, the key evidence of oil and gas accumulation period, is relatively weak. In order to accurately determine the hydrocarbon charging periods of Zhuhai Formation in Wenchang A Sag, the hydrocarbon inclusions and their associated brine inclusions in the sandstone reservoirs of Zhuhai Formation in the study area were taken as the research object. Fluorescence spectroscopy, laser Raman spectroscopy, micro thermometry and other related experiment were used, combined with the analysis of inclusion capture pressure calculation, burial history, paleogeothermal evolution history, and thermal evolution history of hydrocarbon source rocks. The research on hydrocarbon charging stages and their differences in the central depression and the fault zone has been carried out. The results show that there are three kinds of inclusions, including high⁃density single⁃phase oil inclusions, two⁃phase of gas⁃liquid hydrocarbon inclusions and two⁃phase of gas⁃liquid saline inclusions in the sandstonereservoir. The components of hydrocarbon inclusions and the associated brine inclusions are mainly CH4, C2H6, SO2, CO2 and H2O, and the homogenization temperature of brine inclusions distributed mainly from 95 to 180 ℃. Three stages of hydrocarbon filling occurred both in the central depression and the fault zone, but the hydrocarbon filling time is different. The first hydrocarbon charging occurred in the central depression rangesfrom 21.9 to 13.9 Ma, the second oil filling occurred at 12.0 to 8.9 Ma, and the third oil and gas filling occurred at 7.8 to 4.8 Ma. However, in the fault zone, the first oil charging occurred at 21.7 to 10.2 Ma, the second one occurred at 9.1 to 4.9 Ma, and the third oil and gas filling was about 3.9 to 1.5 Ma. The difference of source rock burial depth, multi⁃stage fault activity and their spatio⁃temporal configuration caused by different tectonic subsidence is the main reason for the difference of hydrocarbon generation peak and hydrocarbon accumulation time in the central depression and fault zone. The research results provide a scientific basis forselection and deployment of oil and gas exploration targets in the study area.

       

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