左卫华, 单蕊, 朱伟. 岩性反演在煤层顶板砂体识别中的应用[J]. 煤田地质与勘探, 2018, 46(2): 184-189. DOI: 10.3969/j.issn.1001-1986.2018.02.028
引用本文: 左卫华, 单蕊, 朱伟. 岩性反演在煤层顶板砂体识别中的应用[J]. 煤田地质与勘探, 2018, 46(2): 184-189. DOI: 10.3969/j.issn.1001-1986.2018.02.028
ZUO Weihua, SHAN Rui, ZHU Wei. Application of seismic lithology inversion in identifying sandstone of coalbed roof[J]. COAL GEOLOGY & EXPLORATION, 2018, 46(2): 184-189. DOI: 10.3969/j.issn.1001-1986.2018.02.028
Citation: ZUO Weihua, SHAN Rui, ZHU Wei. Application of seismic lithology inversion in identifying sandstone of coalbed roof[J]. COAL GEOLOGY & EXPLORATION, 2018, 46(2): 184-189. DOI: 10.3969/j.issn.1001-1986.2018.02.028

岩性反演在煤层顶板砂体识别中的应用

Application of seismic lithology inversion in identifying sandstone of coalbed roof

  • 摘要: EXB矿区主要目的层为一套泛滥平原河流相含煤碎屑岩沉积地层,煤层顶板岩性空间变化快,预测难度大。针对该问题,本文利用测井岩石物理分析建立煤、中砂岩、细砂岩和泥质砂岩的波阻抗频率直方图:煤的波阻抗值较小,主要范围3 000~6 300 m/s·(g/cm3);中砂岩的波阻抗值域范围5 500~10 000 m/s·(g/cm3);由于细砂岩和泥质砂岩性质接近,在波阻抗上无法区分,将两者合并处理,值域范围6 000~12 000 m/s·(g/cm3)。然后利用叠后地震反演计算波阻抗体,利用岩相与流体概率分析技术预测煤层顶板岩性的空间展布。结果表明,地震预测的岩性及其厚度的宏观变化趋势与钻井揭示结果基本一致,岩性平面厚度分布规律与沉积环境相符。

     

    Abstract: The main target strata of EXB mining area are a set of flood plain coal-bearing clastic sedimentary strata. The roof lithology of the coal seam changes rapidly and the lithology prediction is difficult. This paper used logging petrophysics analysis to establish the histogram of wave impedance of coal, medium sandstone, fine sandstone and shale sandstone. The impedance of coal was small with an upper limit of 7 500 m/s·(g/cm3). The impedance range of medium sandstone was between 5 500 and 10 000 m/s·(g/cm3). Elastic properties of fine sandstone and shale sandstone were close and indistinguishable in impedance. So the two rocks were merged and their impedance range was 6 000~12 000 m/s·(g/cm3). The seismic impedance volume was calculated by poststack inversion, and the facies and fluids probabilities analysis were applied to predict the spatial distribution of the roof lithology. The result shows that macroscopic change of lithology and its thickness predicted by seismic inversion was consistent with drilling results and lithologically the law of planar distribution of thickness agreed with sedimentary environment.

     

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