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    中国北方六盘山盆地新生界油气包裹体的发现及其油气地质意义

    吴小力 李荣西 胡建民 刘福田 赵帮胜 覃小丽

    吴小力, 李荣西, 胡建民, 刘福田, 赵帮胜, 覃小丽, 2020. 中国北方六盘山盆地新生界油气包裹体的发现及其油气地质意义. 地球科学, 45(1): 303-316. doi: 10.3799/dqkx.2017.577
    引用本文: 吴小力, 李荣西, 胡建民, 刘福田, 赵帮胜, 覃小丽, 2020. 中国北方六盘山盆地新生界油气包裹体的发现及其油气地质意义. 地球科学, 45(1): 303-316. doi: 10.3799/dqkx.2017.577
    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

    中国北方六盘山盆地新生界油气包裹体的发现及其油气地质意义

    doi: 10.3799/dqkx.2017.577
    基金项目: 

    国家自然科学基金项目 41772118

    中央高校基本科研业务费专项资金项目 300102279106

    中央高校基本科研业务费专项资金项目 300102278107

    详细信息
      作者简介:

      吴小力(1989-), 男, 讲师, 从事沉积学及油气成藏地质学研究

    • 中图分类号: P618.13

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

    • 摘要: 在六盘山盆地新生界清水营组石膏中发现了大量的油气包裹体,而油气包裹体的研究对认识盆地新生界油气成藏条件,拓展盆地油气勘探思路具有重要的意义.通过野外地质调查、样品采集和分析测试等手段对清水营组石膏中油气包裹体的发育特征和组成特征进行研究,并开展油源对比,分析油气包裹体中油气的来源和形成过程,探讨了六盘山盆地新生界油气成藏条件和运聚特征.结果表明:清水营组结晶状石膏中油气包裹体中原油来源于清水营组烃源岩;纤维状石膏脉中油气包裹体原油来源于白垩系马东山组烃源岩.六盘山盆地清水营组泥岩具有生烃潜力,是盆地潜在的烃源岩;白垩系烃源岩生成的油气可以沿着断裂等输导体系向上覆地层运移,并在新生界聚集,沟通白垩系烃源岩断层附近的新生界圈闭是六盘山盆地有利的油气聚集区.

       

    • 图  1  六盘山盆地构造位置(a)与地层发育特征(b)

      殷占华和薛萍(2000)修改

      Fig.  1.  Tectonic setting(a) and stratigraphical features(b)of Liupanshan basin

      图  2  六盘山盆地马东山组和清水营组野外露头及岩性特征

      a.清水营组结晶状石膏;b.清水营组纤维状石膏脉;c.清水营组灰绿色薄层状泥岩;d.马东山组灰色泥质灰岩和灰黑色灰质泥岩的互层;e.马东山组灰黑色灰质泥岩

      Fig.  2.  Sections and lithology of Madongshan Formation and Qingshuiying Formation in Liupanshan basin

      图  3  六盘山盆地清水营组石膏中油气包裹体特征

      a1、b1.结晶状石膏,透射光,呈无色透明和褐色的油气包裹体;a2、b2.结晶状石膏,荧光,呈淡蓝色的油气包裹体;c1、d1.纤维状石膏脉,透射光,呈无色透明和褐色的油气包裹体;c2、d2.纤维状石膏脉,荧光,呈淡蓝色的油气包裹体

      Fig.  3.  Characteristic of the hydrocarbon inclusions of Qingshuiying Formation in Liupanshan basin

      图  4  六盘山盆地清水营组石膏中油气包裹体的激光拉曼光谱图

      Fig.  4.  Raman spectrum of the hydrocarbon inclusions in gypsum of Qingshuiying Formation in Liupanshan basin

      图  5  六盘山盆地清水营组石膏中油气包裹体生标化合物质量色谱图

      Fig.  5.  Mass chromatogram of biomarkers of the hydrocarbon inclusions in gypsum of Qingshuiying Formation in Liupanshan basin

      图  6  六盘山盆地清水营组石膏中油气包裹体色质谱分析总离子流图

      Fig.  6.  TICs of hydrocarbon inclusions in gypsum of Qingshuiying Formation in Liupanshan basin

      图  7  样品生物标志化合物油源对比

      Fig.  7.  Oil-source correlation with biomarkers

      图  8  六盘山盆地清水营组石膏中油气包裹体形成过程示意

      Fig.  8.  Forming process of petroleum inclusions in gypsum of Qingshuiying Formation in Liupanshan basin

      表  1  生物标志化合物参数统计表

      Table  1.   Biomarker parameters

      样品 正构烷烃 类异戊二烯烷烃 藿烷 甾烷
      A B C D E F G H I J
      HP40-1 结晶状石膏油包裹体 0.84 0.84 1.08 0.43 0.26 0.30 0.45 0.31 0.23 0.33
      HP42-1 纤维状石膏油包裹体 1.26 0.45 0.53 1.20 0.14 0.44 0.25 0.31 0.45 0.43
      H003 清水营组烃源岩 1.91 0.76 0.88 0.27 0.24 0.37 0.51 0.16 0.33 0.33
      H014 清水营组烃源岩 1.75 0.75 0.94 0.27 0.26 0.40 0.60 0.16 0.24 0.33
      H020 清水营组烃源岩 1.71 0.75 0.90 0.30 0.27 0.41 0.51 0.18 0.31 0.37
      P015 马东山组烃源岩 1.24 0.41 0.56 1.25 0.16 0.87 0.32 0.26 0.42 0.52
      P020 马东山组烃源岩 1.15 0.49 0.48 0.85 0.14 0.82 0.35 0.26 0.39 0.59
      P030 马东山组烃源岩 1.14 0.48 0.42 0.92 0.15 0.82 0.36 0.27 0.37 0.50
      注:A为OEP;B为Pr/Ph;C为Pr/C17;D为Ph/C18;E为伽马蜡烷/C30藿烷;F为Ts/(Ts+Tm);G为C27/(C27+C28+C29)-ααR;H为C28/(C27+C28+C29) -ααR;I为C28/(C27+C28+C29) -ααR;J为甾烷C29-αββ/(αββ+ααα).
      下载: 导出CSV

      表  2  六盘山盆地清水营组石膏中油气包裹体生标化合物热成熟度参数

      Table  2.   Maturity parameters of biomarkers from the fluid inclusions in gypsum of Qingshuiying Formation in Liupanshan basin

      样品 岩性 正构烷烃参数 藿烷参数 甾烷参数 成熟度综合判识
      OEP Ts/(Ts+Tm) C29ββ/(ββ+αα)
      HP40-1 结晶状石膏 0.84 0.30 0.33 未熟‒低熟
      HP42-1 纤维状石膏脉 1.26 0.44 0.43 低熟‒成熟
      下载: 导出CSV

      表  3  六盘山盆地马东山组和清水营组烃源岩有机地化参数

      Table  3.   Organic geochemical parameters of source rocks of Madongshan Formation and Qingshuiying Formation in Liupanshan basin

      样品编号 岩性 地层 TOC(%) S1+S2(mg/g) Tmax(℃) 氯仿沥青“A”(%) Ro (%)
      P015 深灰色灰质泥岩 马东山组 2.72 13.37 467.7 0.60 1.24
      P020 深灰色灰质泥岩 马东山组 1.92 11.73 461.8 0.63 1.11
      P030 深灰色灰质泥岩 马东山组 0.13 0.06 460.5 0.06 1.02
      H003 灰绿色灰质泥岩 清水营组 0.22 0.08 446.8 0.05 0.66
      H014 灰绿色灰质泥岩 清水营组 0.35 0.53 445.2 0.11 0.60
      H020 灰绿色灰质泥岩 清水营组 0.41 0.32 432.2 0.08 0.55
      下载: 导出CSV
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