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湖相烃源岩演化全过程中的孔隙演化机理——基于地质样品与模拟实验的认识

黄振凯 黎茂稳 郑伦举 陶国亮 李志明 蒋启贵 钱门辉 曹婷婷 李双建 沃玉进 孙冬胜

黄振凯, 黎茂稳, 郑伦举, 陶国亮, 李志明, 蒋启贵, 钱门辉, 曹婷婷, 李双建, 沃玉进, 孙冬胜. 湖相烃源岩演化全过程中的孔隙演化机理——基于地质样品与模拟实验的认识[J]. 石油实验地质, 2020, 42(4): 639-645. doi: 10.11781/sysydz202004639
引用本文: 黄振凯, 黎茂稳, 郑伦举, 陶国亮, 李志明, 蒋启贵, 钱门辉, 曹婷婷, 李双建, 沃玉进, 孙冬胜. 湖相烃源岩演化全过程中的孔隙演化机理——基于地质样品与模拟实验的认识[J]. 石油实验地质, 2020, 42(4): 639-645. doi: 10.11781/sysydz202004639
HUANG Zhenkai, LI Maowen, ZHENG Lunju, TAO Guoliang, LI Zhiming, JIANG Qigui, QIAN Menhui, CAO Tingting, LI Shuangjian, WO Yujin, SUN Dongsheng. Pore development in lacustrine source rock evolution: interpretation based on geological samples and simulation experiments: interpretation based on geological samples and simulation experiments[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2020, 42(4): 639-645. doi: 10.11781/sysydz202004639
Citation: HUANG Zhenkai, LI Maowen, ZHENG Lunju, TAO Guoliang, LI Zhiming, JIANG Qigui, QIAN Menhui, CAO Tingting, LI Shuangjian, WO Yujin, SUN Dongsheng. Pore development in lacustrine source rock evolution: interpretation based on geological samples and simulation experiments: interpretation based on geological samples and simulation experiments[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2020, 42(4): 639-645. doi: 10.11781/sysydz202004639

湖相烃源岩演化全过程中的孔隙演化机理——基于地质样品与模拟实验的认识

doi: 10.11781/sysydz202004639
基金项目: 

国家自然科学基金 41702137

中国科学院A类战略性先导科技专项 XDA14010406

国家自然科学基金企业创新发展联合基金项目 U19B6003-01-03

详细信息
    作者简介:

    黄振凯(1985-), 男, 博士, 从事油气地质与地球化学研究。E-mail: huang_zhenkai@163.com

  • 中图分类号: TE122.1

Pore development in lacustrine source rock evolution: interpretation based on geological samples and simulation experiments: interpretation based on geological samples and simulation experiments

  • 摘要: 通过对比实际自然演化剖面地质样品和模拟实验样品的孔隙定量结果,认为烃源岩演化的整个过程中,不同尺度孔隙的孔容变化规律基本相似。大孔和介孔对孔隙变化的影响较大,二者应该是岩石总孔隙度的主要贡献者,且不同尺寸孔隙之间存在一定的转化关系。成岩演化、构造变化等作用是导致孔隙变化的主要外部因素,生烃—排烃过程是内在因素。处于不同演化阶段的烃源岩形成的烃类产物所赋存的孔隙空间及大小(规模)存在一定差异,该认识有助于明确泥页岩层系中不同演化阶段对应的常规与非常规油气资源的赋存机理。

     

  • 图  1  渤海湾盆地东营凹陷取样井位分布

    Figure  1.  Sampling locations in Dongying Sag, Bohai Bay Basin

    图  2  模拟实验条件下泥页岩中不同尺度孔隙的孔容变化特征

    Figure  2.  Variation of volumes of pores with different sizes in shales in simulation experiments

    图  3  模拟实验条件下泥页岩中不同尺度孔隙占比变化特征

    Figure  3.  Variation of proportions of pores with different sizes in shales in simulation experiments

    图  4  模拟实验条件下泥页岩成烃演化特征

    Figure  4.  Hydrocarbon generation of shales in simulation experiments

    图  5  模拟实验条件下泥页岩中气油比变化特征

    Figure  5.  Variation of gas/oil ratios of shales in simulation experiments

    图  6  模拟实验条件下湖相烃源岩微纳米级孔隙演化特征

    Figure  6.  Evolution of micro and nano pores in lacustrine source rocks in simulation experiments

    图  7  渤海湾盆地东营凹陷沙三下亚段与沙四上亚段实际地质剖面样品孔容变化特征

    Figure  7.  Variation of pore volume in actual geological profile samples from the lower third and upper fourth members of Shahejie Formation, Dongying Sag, Bohai Bay Basin

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  • 收稿日期:  2020-03-18
  • 修回日期:  2020-05-22
  • 刊出日期:  2020-07-28

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