Reverse time migration angle gathers in acoustic anisotropic media using direction vectors

IF 3 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Geophysics Pub Date : 2023-12-01 DOI:10.1190/geo2023-0328.1
Kai Yang, Jianfeng Zhang
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引用次数: 0

Abstract

The application of direction vectors in the generation of reverse time migration (RTM) angle gathers in complex acoustic anisotropic media often encounters three main challenges: not pointing to the phase-velocity direction (PVD) of the Poynting vector, inaccuracy due to overlapping wavefields, and instability due to zero points of the direction vector. In general anisotropic media, the normally used Poynting vector indicates the group-velocity direction (GVD), whereas reflection and transmission phenomena rely on the PVD. Anisotropy introduces discrepancies between the GVD and the PVD. To overcome this issue, we employ the so-called PVD vector to directly calculate the PVD from anisotropic wavefields, eliminating the need of the approxi- mated conversion from the GVD to the PVD. To mitigate the inaccuracy problem, we apply the Hilbert transform based wavefield decomposition method to separate over- lapping wavefields into their up/down components, and then we calculate the PVDs using the separated wavefields. To tackle the instability problem, we incorporate the additionally simulated quadrature wavefield during the wavefield decomposition procedure. By combining the direction vector of the quadrature wavefield with that of the original wavefield, we can eliminate the zero points and thus obtain a stabi- lized PVD vector. With those problems solved or alleviated, we present a scheme for the generation of anisotropic RTM angle gathers in complex areas. Two numerical examples utilizing synthetic data sets demonstrate our method’s effectiveness.
利用方向矢量在声学各向异性介质中进行反向时间迁移角度采集
在复杂的声学各向异性介质中应用方向矢量生成反向时间迁移(RTM)角度集合时,经常会遇到三个主要挑战:没有指向 Poynting 矢量的相位速度方向(PVD)、波场重叠导致的不准确性以及方向矢量零点导致的不稳定性。在一般各向异性介质中,通常使用的 Poynting 向量表示群速度方向(GVD),而反射和透射现象则依赖于 PVD。各向异性会造成 GVD 和 PVD 之间的差异。为了解决这个问题,我们采用了所谓的 PVD 向量来直接计算各向异性波场的 PVD,省去了从 GVD 到 PVD 的近似转换。为了缓解不准确问题,我们采用基于希尔伯特变换的波场分解方法,将重叠波场分离为上下分量,然后利用分离后的波场计算 PVD。为了解决不稳定性问题,我们在波场分解过程中加入了额外模拟的正交波场。通过将正交波场的方向矢量与原始波场的方向矢量相结合,我们可以消除零点,从而获得稳定的 PVD 矢量。随着这些问题的解决或缓解,我们提出了在复杂区域生成各向异性 RTM 角集的方案。利用合成数据集的两个数值示例证明了我们方法的有效性。
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来源期刊
Geophysics
Geophysics 地学-地球化学与地球物理
CiteScore
6.90
自引率
18.20%
发文量
354
审稿时长
3 months
期刊介绍: Geophysics, published by the Society of Exploration Geophysicists since 1936, is an archival journal encompassing all aspects of research, exploration, and education in applied geophysics. Geophysics articles, generally more than 275 per year in six issues, cover the entire spectrum of geophysical methods, including seismology, potential fields, electromagnetics, and borehole measurements. Geophysics, a bimonthly, provides theoretical and mathematical tools needed to reproduce depicted work, encouraging further development and research. Geophysics papers, drawn from industry and academia, undergo a rigorous peer-review process to validate the described methods and conclusions and ensure the highest editorial and production quality. Geophysics editors strongly encourage the use of real data, including actual case histories, to highlight current technology and tutorials to stimulate ideas. Some issues feature a section of solicited papers on a particular subject of current interest. Recent special sections focused on seismic anisotropy, subsalt exploration and development, and microseismic monitoring. The PDF format of each Geophysics paper is the official version of record.
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