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基于不同岩性的总有机碳分段预测方法——以东营凹陷始新统沙河街组三段下亚段为例

赵琳洁 陆建林 王保华 李浩 宋振响 张彦霞

赵琳洁, 陆建林, 王保华, 李浩, 宋振响, 张彦霞. 基于不同岩性的总有机碳分段预测方法——以东营凹陷始新统沙河街组三段下亚段为例[J]. 石油实验地质, 2021, 43(4): 721-727. doi: 10.11781/sysydz202104721
引用本文: 赵琳洁, 陆建林, 王保华, 李浩, 宋振响, 张彦霞. 基于不同岩性的总有机碳分段预测方法——以东营凹陷始新统沙河街组三段下亚段为例[J]. 石油实验地质, 2021, 43(4): 721-727. doi: 10.11781/sysydz202104721
ZHAO Linjie, LU Jianlin, WANG Baohua, LI Hao, SONG Zhenxiang, ZHANG Yanxia. Segmented prediction of TOC based on lithology: a case study of the lower sub-member of the third member of the Eocene Shahejie Formation, Dongying Sag, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(4): 721-727. doi: 10.11781/sysydz202104721
Citation: ZHAO Linjie, LU Jianlin, WANG Baohua, LI Hao, SONG Zhenxiang, ZHANG Yanxia. Segmented prediction of TOC based on lithology: a case study of the lower sub-member of the third member of the Eocene Shahejie Formation, Dongying Sag, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(4): 721-727. doi: 10.11781/sysydz202104721

基于不同岩性的总有机碳分段预测方法——以东营凹陷始新统沙河街组三段下亚段为例

doi: 10.11781/sysydz202104721
基金项目: 

中国石化科技部项目“油气战略选区评价与决策支持技术” P21086-1

国家科技重大专项 2017ZX05049001-006

详细信息
    作者简介:

    赵琳洁(1992-), 女, 硕士, 助理工程师, 从事石油地质研究。E-mail: zhaolj.syky@sinopec.com

  • 中图分类号: TE122.115

Segmented prediction of TOC based on lithology: a case study of the lower sub-member of the third member of the Eocene Shahejie Formation, Dongying Sag, Bohai Bay Basin

  • 摘要: 陆相泥页岩具有非均质性强的特征,矿物组分、总有机碳含量(TOC)等参数的分布预测是陆相页岩油气资源评价与选区研究的基础。为获取陆相页岩地层上述关键参数纵向分布特征,克服测试实验周期长、成本高、取样难等现实问题,开展了相应关键参数测井预测方法研究。以渤海湾盆地东营凹陷始新统沙河街组三段下亚段为例,结合XRD实测数据以及测录井等资料,具体针对不同岩性选取不同TOC预测模型,建立了不同岩性的TOC识别模板。运用所构建的模型对Fy1井沙三下亚段的岩性、TOC进行典型预测,分段预测TOC方法得到的预测值与实测值之间的相关系数较高,约为0.84,表明该方法可行性较强,可为开展陆相页岩油资源评价及目标评价提供有效的技术支撑。

     

  • 图  1  渤海湾盆地东营凹陷始新统沙河街组三段下亚段细粒沉积岩岩相分布

    据参考文献[15]。

    Figure  1.  Lithofacies of lamellar fine-grained sedimentary rocks in the lower sub-member of Es3, Dongying Sag, Bohai Bay Basin

    图  2  渤海湾盆地东营凹陷始新统沙河街组三段下亚段岩性三角图

    Figure  2.  Lithology triangular chart of the lower sub-member of Es3, Dongying Sag, Bohai Bay Basin

    图  3  渤海湾盆地东营凹陷始新统沙河街组三段下亚段预测岩性三角图

    Figure  3.  Prediction of lithology of the lower sub-member of Es3, Dongying Sag, Bohai Bay Basin

    图  4  渤海湾盆地东营凹陷始新统沙河街组三段下亚段主要岩性不同方法TOC的预测值与实测值交会图

    Figure  4.  Predicted and measured values of TOC with different methods, lower sub-member of Es3, Dongying Sag, Bohai Bay

    图  5  渤海湾盆地东营凹陷始新统沙河街组三段下亚段黏土岩中AC、DEN曲线与TOC实测值交会图

    Figure  5.  AC, DEN and measured TOC values in clay rocks, lower sub-member of Es3, Dongying Sag, Bohai Bay Basin

    图  6  渤海湾盆地东营凹陷始新统沙河街组三段下亚段不同预测方法预测TOC与实际值交会图

    Figure  6.  Measured and predicted TOC values with different methods, lower sub-member of Es3, Dongying Sag, Bohai Bay Basin

    图  7  渤海湾盆地东营凹陷Fy1井始新统沙河街组三段下亚段柱状图

    Figure  7.  Histogram of lower sub-member of Es3, well Fy1, Dongying Sag, Bohai Bay Basin

    表  1  渤海湾盆地东营凹陷不同岩性的测井响应特征

    Table  1.   Logging responses of different lithologies, Dongying Sag, Bohai Bay Basin

    岩性 测井响应特征 GR/API范围(峰值) AC/(μs·ft-1)范围(峰值) NPHI/%范围(峰值)
    粉砂岩 低GR、低AC、低NPHI 46.49~68.08(59.13) 77.54~95.03(83.55) 0.16~0.26(0.19)
    黏土岩 高GR、高AC、高NPHI 58.08~73.65(64.34) 79.46~97.98(92.92) 0.17~0.25(0.22)
    碳酸盐岩(灰岩) 低GR、中AC、低NPHI 37.81~79.67(59.02) 66.62~113.57(86.15) 0.12~0.33(0.19)
    混合细粒岩 中GR、中AC、中NPHI 36.99~87.06(60.17) 66.04~111.01(88.91) 0.12~0.33(0.20)
    下载: 导出CSV

    表  2  渤海湾盆地东营凹陷始新统沙河街组三段下亚段不同岩性TOC预测模型

    Table  2.   Prediction models of TOC of different lithologies, lower sub-member of Es3, Dongying Sag, Bohai Bay Basin

    岩性 TOC预测方法 预测模型及参数
    混合细粒岩 密度曲线法 $ \omega(\mathrm{TOC})=a_1 D E N+b_1$
    灰岩 密度曲线法 $ \omega(\mathrm{TOC})=a_2 D E N+b_2$
    粉砂岩 ΔlogR $ \Delta \lg R=\lg \left(\frac{R}{2.213}\right)+0.02(\Delta t-75.013)$
    $ \omega(\mathrm{TOC})=10^{(2.297-0.1688 \mathrm{LOM})} \Delta \lg R+c_3$
    泥岩 多元回归法 $ \omega(\mathrm{TOC})=a_4 D E N+b_4 A C+c_4 G R+d_4$
    注:DEN为密度曲线;R为电阻率曲线;Δt为声波时差曲线;LOM为成熟度指数;a1a2a4b4c4为斜率;b1b2c3d4为截距。
    下载: 导出CSV
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  • 收稿日期:  2020-04-28
  • 修回日期:  2021-06-04
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