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低钻揭洼陷有利烃源岩空间展布地质与地球物理综合识别方法——以珠江口盆地珠一坳陷恩平17洼为例

彭光荣 龙祖烈 史玉玲 石创 杨兴业 刘灵 马晓楠

彭光荣, 龙祖烈, 史玉玲, 石创, 杨兴业, 刘灵, 马晓楠. 低钻揭洼陷有利烃源岩空间展布地质与地球物理综合识别方法——以珠江口盆地珠一坳陷恩平17洼为例[J]. 石油实验地质, 2022, 44(6): 1116-1122. doi: 10.11781/sysydz2022061116
引用本文: 彭光荣, 龙祖烈, 史玉玲, 石创, 杨兴业, 刘灵, 马晓楠. 低钻揭洼陷有利烃源岩空间展布地质与地球物理综合识别方法——以珠江口盆地珠一坳陷恩平17洼为例[J]. 石油实验地质, 2022, 44(6): 1116-1122. doi: 10.11781/sysydz2022061116
PENG Guangrong, LONG Zulie, SHI Yuling, SHI Chuang, YANG Xingye, LIU Ling, MA Xiaonan. Discussion on integrated geological and geophysical identification method for spatial distribution of favorable source rocks in depression with lack of drilling data: a case study of Enping 17 Sag, Zhu Ⅰ Depression, Pearl River Mouth Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(6): 1116-1122. doi: 10.11781/sysydz2022061116
Citation: PENG Guangrong, LONG Zulie, SHI Yuling, SHI Chuang, YANG Xingye, LIU Ling, MA Xiaonan. Discussion on integrated geological and geophysical identification method for spatial distribution of favorable source rocks in depression with lack of drilling data: a case study of Enping 17 Sag, Zhu Ⅰ Depression, Pearl River Mouth Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(6): 1116-1122. doi: 10.11781/sysydz2022061116

低钻揭洼陷有利烃源岩空间展布地质与地球物理综合识别方法——以珠江口盆地珠一坳陷恩平17洼为例

doi: 10.11781/sysydz2022061116
基金项目: 

中海石油深海开发有限公司项目 KJZH-2021-0003-00

中国海洋石油集团有限公司重大科技项目 KJGG2022-0403

详细信息
    作者简介:

    彭光荣(1978—),男,硕士,高级工程师,从事油气地质与油气勘探综合研究工作。E-mail:penggr@cnooc.com.cn

    通讯作者:

    史玉玲(1987—),女,硕士,工程师,从事资源评价和油气运移成藏研究工作。E-mail:shiyl5@cnooc.com.cn

  • 中图分类号: TE122.1

Discussion on integrated geological and geophysical identification method for spatial distribution of favorable source rocks in depression with lack of drilling data: a case study of Enping 17 Sag, Zhu Ⅰ Depression, Pearl River Mouth Basin

  • 摘要: 为解决珠江口盆地珠一坳陷低钻揭洼陷有利烃源岩展布的综合识别问题,以珠江口盆地珠一坳陷恩平17洼为例,在对烃源岩发育地质背景、沉积特征及岩石物理特征分析的基础上,以不同沉积环境烃源岩的岩石物理特征约束指导地震反演;根据钻揭烃源岩岩相与反演阻抗体关系统计,通过地质建模进行有利烃源岩空间展布的半定量预测;结合原油的地化成因类型及来源认识分析预测方法及结果的合理性,探讨低钻揭洼陷有利烃源岩空间展布的地质与地球物理综合识别方法。古近系文昌组烃源岩沉积环境越好,有利烃源岩段的阻抗值越低,与差烃源岩或非烃源岩段之间的阻抗差异越大。从预测结果看,文三段、文四段及文五段是恩平17洼的主力烃源岩段,这一认识得到了原油生物标志化合物研究的支持。在石油地质背景条件基本明确的珠江口盆地各小洼陷,建立烃源岩岩相与反演阻抗值之间的定量、半定量关系,有助于快速明确主力烃源岩发育层段及规模,这一方法具有较好的推广应用前景。

     

  • 图  1  珠江口盆地珠一坳陷恩平17洼构造位置及地层柱状图

    Figure  1.  Structural location and stratigraphic histogram of Enping 17 Sag, Zhu Ⅰ Depression, Pearl River Mouth Basin

    图  2  珠江口盆地珠一坳陷恩平17洼E4井文昌组岩性组合及其测井响应特征

    Figure  2.  Lithology combination and logging response characteristics of Wenchang Formation in well E4, Enping 17 Sag, Zhu Ⅰ Depression, Pearl River Mouth Basin

    图  3  珠江口盆地珠一坳陷恩平17洼过E4井纵测线方向反演波阻抗剖面

    剖面位置见图 1aAA

    Figure  3.  Inversion wave impedance profile in the direction of longitudinal survey line through well E4, Enping 17 Sag, Zhu Ⅰ Depression, Pearl River Mouth Basin

    图  4  珠江口盆地珠一坳陷恩平17洼E4井古近系文昌组砂泥岩反演阻抗值分布

    Figure  4.  Inversion impedance values of sandstones and mudstones in Wenchang Formation of well E4, Enping 17 Sag, Zhu Ⅰ Depression, Pearl River Mouth Basin

    图  5  珠江口盆地珠一坳陷恩平17洼文昌组有利烃源岩厚度分布

    Figure  5.  Thickness distribution of favorable source rocks of Wenchang Formation in Enping 17 Sag, Zhu Ⅰ Depression, Pearl River Mouth Basin

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  • 收稿日期:  2022-05-25
  • 修回日期:  2022-09-26
  • 刊出日期:  2022-11-28

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