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Poynting and polarization vectors based wavefield decomposition and their application on elastic reverse time migration in 2D transversely isotropic media

机译:基于Poynting和极化矢量的波场分解及其在二维横观各向同性介质中的弹性逆时偏移中的应用

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摘要

With the progress in computational power and seismic acquisition, elastic reverse time migration is becoming increasingly feasible and helpful in characterizing the physical properties of subsurface structures. To achieve high-resolution seismic imaging using elastic reverse time migration, it is necessary to separate the compressional (P-wave) and shear (S-wave) waves for both isotropic and anisotropic media. In elastic isotropic media, the conventional method for wave-mode separation is to use the divergence and curl operators. However, in anisotropic media, the polarization direction of P waves is not exactly parallel to the direction of wave propagation. Also, the polarization direction of S-waves is not totally perpendicular to the direction of wave propagation. For this reason, the conventional divergence and curl operators show poor performance in anisotropic media. Moreover, conventional methods only perform well in the space domain of regular grids, and they are not suitable for elastic numerical simulation algorithms based on non-regular grids. Besides, these methods distort the original wavefield by taking spatial derivatives. In this case, a new anisotropic wave-mode separation scheme is developed using Poynting vectors. This scheme can be performed in the angle domain by constructing the relationship between group and polarization angles of different wave modes. Also, it is performed pointwise, independent of adjacent space points, suitable for parallel computing. Moreover, there is no need to correct the changes in phase and amplitude caused by the derivative operators. By using this scheme, the anisotropic elastic reverse time migration is more efficiently performed on the unstructured mesh. The effectiveness of our scheme is verified by several numerical examples.
机译:随着计算能力和地震采集的进步,弹性逆时偏移正变得越来越可行,并有助于表征地下结构的物理特性。为了使用弹性逆时偏移实现高分辨率地震成像,对于各向同性和各向异性介质,有必要分离压缩波(P波)和剪切波(S波)。在弹性各向同性介质中,波模式分离的常规方法是使用发散和卷曲运算符。但是,在各向异性介质中,P波的偏振方向并不完全与波的传播方向平行。另外,S波的偏振方向也不完全垂直于波的传播方向。因此,常规的发散和卷曲算子在各向异性介质中显示出较差的性能。而且,常规方法仅在规则网格的空间域中表现良好,并且不适用于基于非规则网格的弹性数值模拟算法。此外,这些方法通过采用空间导数来扭曲原始波场。在这种情况下,使用Poynting向量开发了一种新的各向异性波模式分离方案。通过构造不同波模式的群角和偏振角之间的关系,可以在角度域中执行该方案。而且,它独立于相邻空间点逐点执行,适合并行计算。而且,不需要校正由导数算子引起的相位和幅度的变化。通过使用此方案,可以在非结构化网格上更有效地执行各向异性弹性逆向时间偏移。通过几个数值例子验证了我们方案的有效性。

著录项

  • 来源
    《Geophysical Prospecting》 |2019年第5期|1296-1311|共16页
  • 作者单位

    Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China|Southern Univ Sci & Technol, Dept Earth & Space Sci, Shenzhen 518055, Peoples R China;

    King Abdullah Univ Sci & Technol, Thuwal 23955, Saudi Arabia;

    Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China;

    Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Unstructured mesh; Elastic reverse time migration; Anisotropic wave-mode separation; Poynting vectors;

    机译:非结构网格弹性逆时偏移各向异性波模分离坡印廷矢量;
  • 入库时间 2022-08-18 04:18:20

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