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叠前反演方法在致密砂岩气储层预测中的应用

薛明喜 陈开远 田泽华 贾曙光

薛明喜, 陈开远, 田泽华, 等, 2018. 叠前反演方法在致密砂岩气储层预测中的应用. 地质力学学报, 24 (1): 42-50. DOI: 10.12090/j.issn.1006-6616.2018.24.01.005
引用本文: 薛明喜, 陈开远, 田泽华, 等, 2018. 叠前反演方法在致密砂岩气储层预测中的应用. 地质力学学报, 24 (1): 42-50. DOI: 10.12090/j.issn.1006-6616.2018.24.01.005
XUE Mingxi, CHEN Kaiyuan, TIAN Zehua, et al., 2018. APPLICATION OF PRESTACK INVERSION METHOD IN THE PREDICTION OF TIGHT SANDSTONE GAS RESERVOIR. Journal of Geomechanics, 24 (1): 42-50. DOI: 10.12090/j.issn.1006-6616.2018.24.01.005
Citation: XUE Mingxi, CHEN Kaiyuan, TIAN Zehua, et al., 2018. APPLICATION OF PRESTACK INVERSION METHOD IN THE PREDICTION OF TIGHT SANDSTONE GAS RESERVOIR. Journal of Geomechanics, 24 (1): 42-50. DOI: 10.12090/j.issn.1006-6616.2018.24.01.005

叠前反演方法在致密砂岩气储层预测中的应用

doi: 10.12090/j.issn.1006-6616.2018.24.01.005
基金项目: 

国家"十三五"重大专项"薄层地震波场特征与反演研究"专题 2016ZX05002-005-008

详细信息
    作者简介:

    薛明喜(1986-), 男, 博士研究生, 主要从事石油天然气勘探及储层预测工作。E-mail:xuemingxi@163.com

  • 中图分类号: P618.13;P628.2

APPLICATION OF PRESTACK INVERSION METHOD IN THE PREDICTION OF TIGHT SANDSTONE GAS RESERVOIR

  • 摘要: 以鄂尔多斯东缘A区块为例,通过岩石物理正演分析,论证了储层岩石物理参数的敏感性,确定利用纵波阻抗与纵横波速度比参数进行储层的识别。在此基础上进行正演模拟,研究了地震的极限分辨率及不同厚度砂体的地震响应特征,确定了运用叠前地质统计学反演为核心的储层预测技术对该研究区太原组进行储层预测研究,以解决该区储层薄、横向变化快、单一岩石物理参数无法区分岩性等问题。地质统计学反演结果表明,该方法能有效的预测厚度大于3 m的储层。对比研究区内11口测井解释厚度与储层反演厚度表明,储层反演预测厚度平均误差为7.5%,其中5口盲井的平均误差为10.2%,一口新钻井的砂体厚度预测误差为1.73%,为该区的井位部署提供了可靠的资料参考。

     

  • 图  1  鄂尔多斯东缘A区块太原组连井对比剖面

    Figure  1.  Correlation section of Taiyuan formation in A block, eastern margin of the Ordos basin

    图  2  太原组岩石弹性参数分岩性统计结果

    Figure  2.  Lithology statistics of rock elastic parameters of Taiyuan formation

    图  3  地震资料品质分析

    Figure  3.  Seismic data quality analysis

    图  4  井地震正演模拟剖面

    a—地质模型; b—实际地震剖面; c—正演地震剖面; d—正演同时反演剖面

    Figure  4.  Section of seismic forward modeling

    图  5  道集优化处理

    Figure  5.  Optimization progress of gathers

    图  6  太原组岩相概率(a)及所占比例(b)

    Figure  6.  Lithofacies probability and ratio of Taiyuan formation

    图  7  A-5、A-4、A-6井纵、横波速度比对比剖面

    a—叠前同时反演剖面; b—叠前地质统计学反演剖面

    Figure  7.  Correlation profiles of Vp/Vs in A-5, A-4, A-6 well

    图  8  过A-6井地质统计学反演剖面

    Figure  8.  Pre-stack geostatistical inversion section of A-6 well

    图  9  A区块叠前地质统计学反演厚度验证

    Figure  9.  Thickness verification of pre-stack geostatistical inversion in A block

    表  1  正演模型参数表

    Table  1.   Forward model parameters

    编号 厚度/m 纵波阻抗/g·cm-3·m·s-1 纵横波速度比 密度/g·cm-3
    1号砂体 3.2 10220 1.71 2.52
    2号砂体 12 9855 1.69 2.50
    3号砂体 4.1 10060 1.70 2.51
    泥岩 12600 1.90 2.69
    下载: 导出CSV

    表  2  研究区太原组各岩性弹性参数XYZ方向变程

    Table  2.   X/Y/Z direction variable range of different lithologies of Taiyuan formation

    岩性 X/m Y/m Z/ms
    砂岩 1200 1200 1
    泥岩 1600 1600 2
    1000 1000 4
    下载: 导出CSV

    表  3  A-6井太原组砂体预测精度对比

    Table  3.   Sand body prediction accuracy comparison in Taiyuan formation of A-6 well

    砂体编号 测井厚度/m 反演厚度/m 误差/% 备注
    1 4.26 3.2 24.8 含0.4 m泥岩夹层
    2 2.2 0
    3 5.0 4.3 14
    4 2.8 0
    5 1.4 0
    6 1.3 0
    7 5.0 5.6 12 含0.1 m泥岩夹层
    8 1.5 0
    9 1.5 0
    下载: 导出CSV

    表  4  叠前地质统计学反演误差统计表

    Table  4.   Error statistics of pre-stack geostatistical inversion

    井名 层位 钻井砂厚/m 预测砂厚/m 误差率/%
    A-4 T2 23.20 21.66 6.64
    A-5 T2 6.40 6.37 0.50
    A-6 T2 15.00 14.85 1.02
    A-8 T2 3.80 4.86 27.95
    A-15 T2 4.10 4.31 5.18
    A-16 T2 3.40 3.11 8.50
    A-20 T2 20.70 20.40 1.46
    A-26 T2 9.90 9.81 0.94
    A-28 T2 24.00 22.46 6.40
    A-101 T2 22.40 22.01 1.73
    A-105 T2 13.40 15.45 15.29
    误差均值: 7.5
    注:A-8、A-15、A-26、A-101、A-105井均未参与反演约束
    下载: 导出CSV
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  • 收稿日期:  2017-09-15
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