粘弹性各向异性介质的波场分解

GEOPHYSICS Pub Date : 2024-04-01 DOI:10.1190/geo2023-0583.1
Qi Hao, I. Tsvankin
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引用次数: 0

摘要

分离地震记录上的波模式是多分量地震数据成像的重要步骤。粘弹性各向异性模型可真实描述速度和衰减均呈现各向异性的地下构造。然而,模式分离尚未扩展到粘弹性各向异性介质。在这里,我们提出了一种有效的波场分解方法,它同时考虑了速度和衰减的各向异性。我们的算法在频率-波数域运行,因此适用于一般耗散模型。我们提出了在任意各向异性衰减均质介质中进行波场分解的精确方程。然后,将提出的方法应用于粘弹性恒定 Q VTI(具有垂直对称轴的横向各向同性)模型。数值示例证明了我们的方法对于速度和衰减各向异性明显的片状均质介质的准确性和效率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Wavefield decomposition for viscoelastic anisotropic media
Separating wave modes on seismic records is an essential step in imaging of multicomponent seismic data. Viscoelastic anisotropic models provide a realistic description of subsurface formations that exhibit anisotropy of both velocity and attenuation. However, mode separation has not been extended to viscoelastic anisotropic media yet. Here, we propose an efficient approach to wavefield decomposition that takes both velocity and attenuation anisotropy into account. Our algorithm operates in the frequency-wavenumber domain and, therefore, is suitable for general dissipative models. We present exact equations for wavefield decomposition in arbitrarily anisotropic attenuative homogeneous media. Then the proposed approach is applied to viscoelastic constant- Q VTI (transversely isotropic with a vertical symmetry axis) models. Numerical examples demonstrate the accuracy and efficiency of our approach for piecewise-homogeneous media characterized by pronounced velocity and attenuation anisotropy.
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