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渤海湾盆地渤中凹陷西南部深层烃源岩有机相预测

王祥 马劲风 王飞龙 王震亮 陈容涛 闫昕宇

王祥, 马劲风, 王飞龙, 王震亮, 陈容涛, 闫昕宇. 渤海湾盆地渤中凹陷西南部深层烃源岩有机相预测[J]. 石油实验地质, 2022, 44(6): 1070-1080. doi: 10.11781/sysydz2022061070
引用本文: 王祥, 马劲风, 王飞龙, 王震亮, 陈容涛, 闫昕宇. 渤海湾盆地渤中凹陷西南部深层烃源岩有机相预测[J]. 石油实验地质, 2022, 44(6): 1070-1080. doi: 10.11781/sysydz2022061070
WANG Xiang, MA Jinfeng, WANG Feilong, WANG Zhenliang, CHEN Rongtao, YAN Xinyu. Prediction of organic facies of deep source rocks in southwestern part of Bozhong Sag, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(6): 1070-1080. doi: 10.11781/sysydz2022061070
Citation: WANG Xiang, MA Jinfeng, WANG Feilong, WANG Zhenliang, CHEN Rongtao, YAN Xinyu. Prediction of organic facies of deep source rocks in southwestern part of Bozhong Sag, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(6): 1070-1080. doi: 10.11781/sysydz2022061070

渤海湾盆地渤中凹陷西南部深层烃源岩有机相预测

doi: 10.11781/sysydz2022061070
基金项目: 

中海石油(中国)有限公司天津分公司课题“渤中凹陷深层成烃成藏机理与规律研究” CCL2018TJTZDST0579

详细信息
    作者简介:

    王祥(1997—),男,硕士研究生,从事烃源岩地球物理预测研究。E-mail:wangxiang1@stumail.nwu.edu.cn

    通讯作者:

    马劲风(1965—),男,教授,博士生导师,从事地震勘探和储层预测等研究。E-mail:jinfengma@sina.com

  • 中图分类号: TE122.113

Prediction of organic facies of deep source rocks in southwestern part of Bozhong Sag, Bohai Bay Basin

  • 摘要: 针对渤海湾盆地渤中凹陷西南部烃源岩层系多、非均质性较强等特点,开展了烃源岩干酪根显微组分、元素分析、岩石热解、气相色谱等地球化学分析测试,在沉积相的约束下对比了ΔlogR系列方法、多元回归法、BP神经网络法预测有机质丰度参数的优劣,优选BP神经网络法进行烃源岩总有机碳含量、裂解烃含量的单井预测,进而计算得到氢指数预测曲线,结合总有机碳含量进行有机相分析,定量刻画各层系烃源岩的有机相,分析烃源岩的优劣和展布特征。结果表明,BP神经网络法的预测精度相对较高,东营组二段下亚段烃源岩主要为Ⅱ2型干酪根,氢指数为125~400 mg/g,总有机碳含量基本小于3%,其有机相主要为BC相、C相和CD相;东营组三段烃源岩主要为Ⅱ1—Ⅱ2型干酪根,沙河街组沙一二段、沙三段烃源岩主要为Ⅰ—Ⅱ1型干酪根,这三套烃源岩的氢指数为250~650 mg/g,总有机碳含量为3%左右或大于3%,其有机相主要为B相、BC相和C相。沙河街组优质烃源岩主要发育于研究区中南部,是下一步勘探的重点区域。

     

  • 图  1  渤海湾盆地渤中凹陷区域概况(a)、研究区位置(b)及地层综合柱状图(c)

    据文献[19, 37]修改。

    Figure  1.  Regional overview of Bozhong Sag (a), location of study area (b), and generalized stratigraphic histogram (c), Bohai Bay Basin

    图  2  渤海湾盆地渤中凹陷西南部烃源岩干酪根显微组分(a)、干酪根H/C原子比和O/C原子比(b)、TOC含量(c)和Pr/nC17和Ph/nC18值相关图(d)

    Figure  2.  Microscopic composition of kerogen (a), H/C and O/C ratio of kerogen (b), TOC content (c), and correlation between Pr/nC17 and Ph/nC18 (d) of source rocks from southwestern part of Bozhong Sag, Bohai Bay Basin

    图  3  渤海湾盆地渤中凹陷西南部烃源岩岩石热解氢指数、总有机碳含量、生烃潜力交会图

    Figure  3.  Intersection of pyrolysis hydrogen index, TOC content and S1+S2 of source rocks from southwestern part of Bozhong Sag, Bohai Bay Basin

    图  4  渤海湾盆地渤中凹陷西南部烃源岩测井参数与TOC、S2交会图

    Figure  4.  Intersection of logging parameters and TOC and S2 of source rocks from southwestern part of Bozhong Sag, Bohai Bay Basin

    图  5  三层BP神经网络预测TOC、S2原理

    Figure  5.  Schematic diagram of TOC and S2 prediction by three-layer BP neural network

    图  6  四种方法预测TOC判定系数R2、平均相对误差分析

    Figure  6.  Coefficient R2 and average relative error of four methods for TOC prediction

    图  7  渤海湾盆地渤中凹陷西南部Q3井TOC、S2IH预测与实测综合地球化学剖面

    Figure  7.  Generalized geochemical profiles showing predicted and measured TOC, S2, and IH values of well Q3, southwestern part of Bozhong Sag, Bohai Bay Basin

    图  8  渤海湾盆地渤中凹陷西南部烃源岩沉积相和各有机相分布

    a.E3d2L沉积相;b.E3d3沉积相;c.E2s1+2沉积相;d.E2s3沉积相;e.E3d2LC相;f.E3d3B相;g.E2s1+2B相;h.E2s3B相;i.E3d2LCD相;j.E3d3BC相;k.E2s1+2BC相;l.E2s3BC相

    Figure  8.  Sedimentary facies and organic facies distribution of source rocks in southwestern part of Bozhong Sag, Bohai Bay Basin

    表  1  有机相分类

    Table  1.   Classification of organic facies

    表  2  渤海湾盆地渤中凹陷西南部各TOC预测方法判定系数R2对比

    Table  2.   Coefficient R2 calculated by various methods for TOC prediction, southwestern part of Bozhong Sag, Bohai Bay Basin

    层位 沉积相 ΔlogR 广义ΔlogR 多元回归法 BP神经网络法
    E3d2L 辫状河三角洲 0.712 3 0.722 7 0.818 1 0.933 5
    滨浅湖 0.780 6 0.800 3 0.581 4 0.878 9
    半深湖—深湖 0.008 8 0.321 5 0.322 3 0.839 2
    湖底扇 0.220 0 0.592 4 0.609 6 0.890 2
    E3d3 滨浅湖 0.550 6 0.818 1 0.719 8 0.804 1
    半深湖—深湖 0.346 0 0.580 2 0.705 9 0.891 1
    E2s1+2 滨浅湖 0.312 5 0.469 5 0.347 7 0.862 5
    E2s3 半深湖—深湖 0.215 3 0.433 4 0.325 5 0.743 2
    辫状河三角洲 0.558 3 0.693 2 0.700 9 0.811 3
    下载: 导出CSV
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出版历程
  • 收稿日期:  2021-07-29
  • 修回日期:  2022-09-28
  • 刊出日期:  2022-11-28

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