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    辽河盆地西部凹陷原油的生物标志物类型及其地球化学意义

    朱芳冰 周红

    朱芳冰, 周红, 2018. 辽河盆地西部凹陷原油的生物标志物类型及其地球化学意义. 地球科学, 43(2): 594-598. doi: 10.3799/dqkx.2018.027
    引用本文: 朱芳冰, 周红, 2018. 辽河盆地西部凹陷原油的生物标志物类型及其地球化学意义. 地球科学, 43(2): 594-598. doi: 10.3799/dqkx.2018.027
    Zhu Fangbing, Zhou Hong, 2018. Boimarker Types and Geochemical Significance of Crude Oils in Western Depression, Liaohe Basin. Earth Science, 43(2): 594-598. doi: 10.3799/dqkx.2018.027
    Citation: Zhu Fangbing, Zhou Hong, 2018. Boimarker Types and Geochemical Significance of Crude Oils in Western Depression, Liaohe Basin. Earth Science, 43(2): 594-598. doi: 10.3799/dqkx.2018.027

    辽河盆地西部凹陷原油的生物标志物类型及其地球化学意义

    doi: 10.3799/dqkx.2018.027
    基金项目: 

    国家自然科学基金重大项目 41690130

    详细信息
      作者简介:

      朱芳冰(1966-), 女, 副教授, 主要从事石油地质与油藏工程的教学与科研工作

    • 中图分类号: P618.13

    Boimarker Types and Geochemical Significance of Crude Oils in Western Depression, Liaohe Basin

    • 摘要: 原油的生物标志物组合特征可提供油气来源、成熟度、次生改造程度等多方面的重要信息,是油气成因分析和油源对比的有效工具.利用原油的生物标志物类型及其组合特征分析地球化学意义,通过生物降解作用的研究和原油生物标志物组合的判断,对稠油的来源进行成因分析,研究认为:辽河盆地不同地区各类生物标志物的组合及正构烷烃和异戊间二烯的分布特征,反映研究区发育母质输入、成熟度和生物降解程度明显不同的两种类型的原油,即富4-甲基甾烷型和富伽马蜡烷型原油,分别来源于沙三段和沙四段源岩.

       

    • 图  1  辽河盆地原油甾烷构成三角图

      Fig.  1.  Crude oil sterane constitution triangular figure in the Western depression, Liaohe basin

      图  2  辽河盆地西部凹陷原油和生油岩C29甾烷20S/(S+R)与C29甾烷ββ/(ββ+αα)(a)及Ts/Tm(b)的关系

      Fig.  2.  The relationship between C29 sterane 20S/(S+R) and C29 sterane ββ/(ββ+αα)(a) as well as Ts/Tm (b) in the Western depression, Liaohe basin

      图  3  辽河盆地西部凹陷原油和生油岩C27重排甾烷与4-甲基甾烷/(4-甲基甾烷+C29甾烷ααR)的关系

      Fig.  3.  The relationship between crude oil and source rock C27 rearranged sterane and 4-methylsterane/ (4-methylsterane+C29 sterane ααR) in the Western depression, Liaohe basin

      图  4  辽河盆地西部凹陷未成熟油甾萜生物标志物分布及其与沙四段源岩的对比

      Fig.  4.  The distribution of immature crude steroid terpene biomarker and Sha 4 oil-source correlation in the Western Depression, Liaohe Basin

      图  5  富4-甲基型原油与沙三段源岩的甾萜类生物标志物分布

      Fig.  5.  Rich 4-methyl crude oil and the distribution of Sha 3 source rock steroid terpene biomarker

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      [2] Dong, C.M., 1995.Biological Marker of Crude Oil and Source Rock in Liaodong Gulf.Journal of the University of Petroleum, China, 19(2):12-18 (in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/S0146638097000284
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      [5] Li, S.F., Hu, S.Z., He, S., et al., 2010.Oil-Source Correlation for Biodegraded Oils in the North Slope of the Biyang Depression.Acta Petrolei Sinica, 31(6):946-951(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB201006013.htm
      [6] Peter, K.E., Moldowan, J.M, 1993.The Boimarker Guide:Englewood Cliffs.Prentice Hall, New Jersery, 363. http://www.oalib.com/references/15771495
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      [9] Zhang, L.Y., Liu, Q., Zhang, C.R., 2005.The Relationship Research between Hydrocarbon Generation and Accumulation in Dongying Depression.Geological Publishing House, Beijing, 202(in Chinese).
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      [11] Zhu, Y.M., Weng, H.X., Su, A.G., et al., 2005.Geochemical Characteristics of Tertiary Saline Lacustrine Oils in the Western Qaidam Basin, Northwest China.Applied Geochemistry, 20(10):1875-1889. https://doi.org/10.1016/j.apgeochem.2005.06.003
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    出版历程
    • 收稿日期:  2017-07-23
    • 刊出日期:  2018-02-15

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