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Seismic inversion modeling method for faulted basins:a case study of Liaohe Beach in Bijialing region

机译:断裂盆地的地震反演模拟方法-以毕家岭地区辽河滩为例

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摘要

There is not much correlation between sand content and P-wave impedance in faulted basins , and the prediction results cannot be guaranteed .Due to sedimentary facies control , there is inconsistency between sand content and low frequency trend of P-wave impedance , causing problems for seismic inversion modeling , which directly affects final seismic inversion results .The acoustic impedance increases with burial depth .When the same layers of sand and shale formation endure different compaction , the acoustic impedance values will be dif-ferent .Therefore , The seismic inversion modeling of faulted basin is different from that of conventional basins . The authors built an inversion model using uncompact sandstone percentage , directly compensating for the low frequency trend of the inversion model .In addition, the model's intermediate frequency is similar to P-wave im-pedance , ensuring that the inversion results are converged correctly .The final results of the inversion can be used directly as sandstone percentage .The aforementioned method was applied to Liaohe Beach in the Bijialing region and obtained optimistic lithology inversion effects:the results were correlated well with the depositional facies map and with lithology in the well borehole .The inversion results can be used to define the sand body horizontally and can separate sand bodies vertically , which is very difficult on conventional seismic section . Therefore the inversion results played an important role in reservoir prediction .
机译:断层盆地的含砂量与纵波阻抗之间没有太大的相关性,也不能保证预测结果。由于沉积相控制,含砂量与纵波阻抗的低频趋势不一致,导致了问题。地震反演模型直接影响最终的地震反演结果。声阻抗随埋藏深度的增加而增加。当同一层砂页岩地层承受不同的压实度时,声阻抗值会有所不同。断层盆地与常规盆地不同。作者使用不紧实的砂岩百分比建立了一个反演模型,直接补偿了该反演模型的低频趋势,此外,该模型的中频类似于P波阻抗,确保了反演结果正确收敛。反演的最终结果可以直接作为砂岩的百分比。上述方法应用于毕家岭地区的辽河滩,获得了乐观的岩性反演效果:其结果与沉积相图和井眼的岩性密切相关。反演结果可用于水平界定砂体,垂直分离砂体,这在传统地震剖面上很难实现。因此反演结果在储层预测中发挥了重要作用。

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  • 来源
    《世界地质(英文版)》 |2017年第4期|253-258|共6页
  • 作者

    JING Siliang; LU Qi; WANG Dian;

  • 作者单位

    College of Geo-exploration Science and Technology, Jilin University, Changchun 130026, China;

    College of Geo-exploration Science and Technology, Jilin University, Changchun 130026, China;

    College of Geo-exploration Science and Technology, Jilin University, Changchun 130026, China;

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