Q-compensated image-domain least-squares reverse time migration through preconditioned point-spread functions

IF 3 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Geophysics Pub Date : 2024-03-22 DOI:10.1190/geo2023-0333.1
Wei Zhang, Jinghuai Gao, Ying Shi, Xuan Ke, Zhen Li, Tao Yang, Wenbo Sun
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引用次数: 0

Abstract

Image-domain least-squares reverse time migration (IDLSRTM) through point-spread functions (PSFs) has been proven to be a feasible approach to improve the spatial resolution and amplitude fidelity of reflection images recovered by reverse time migration (RTM). However, it usually ignores the earth’s Q-effects, which may lead to an unfocused reflection image with an undesired spatial resolution. In this paper, we develop a Q-compensated IDLSRTM approach (denoted as Q-IDLSRTM) through PSFs, in which we use the viscoacoustic wave equation based on the generalized standard linear solid model to simulate inherent subsurface attenuation and the linear inversion to compensate for the amplitude attenuation. The PSFs are estimated by a round of modeling-migration computation and spatial interpolation on the fly. There are two key points in the developed Q-IDLSRTM approach. The first is that we must apply the deblurring filter as a preconditioner to compensate for the attenuation of image amplitude of PSFs and RTM in a viscoacoustic medium, before the iterative solution. The preconditioned PSFs and RTM images can help us to construct a less ill-posed image-domain inverse problem that can produce an improved image quality and a faster convergence rate, compared with the conventional Q-IDLSRTM approach without the deblurring filter. The second key point is that we can impose the L1-norm constraint and total variation regularization on the reflection image to stabilize the solution of the ill-posed inverse problem. Several 2D and 3D experiments verify that the developed approach can achieve better imaging quality in terms of amplitude fidelity and spatial resolution relative to the conventional Q-IDLSRTM and acoustic IDLSRTM approaches.
通过预处理点展函数实现 Q 补偿图像域最小二乘反向时间迁移
通过点分布函数(PSF)进行图像域最小二乘反向时间迁移(IDLSRTM)已被证明是提高反向时间迁移(RTM)恢复的反射图像的空间分辨率和振幅保真度的可行方法。然而,它通常会忽略地球的 Q 值效应,这可能会导致反射图像不聚焦,空间分辨率不理想。本文通过 PSFs 开发了一种 Q 补偿 IDLSRTM 方法(称为 Q-IDLSRTM),其中我们使用基于广义标准线性固体模型的粘声波方程来模拟固有的地下衰减,并使用线性反演来补偿振幅衰减。PSF 是通过一轮建模-迁移计算和空间插值来估算的。所开发的 Q-IDLSRTM 方法有两个关键点。首先,在迭代求解之前,我们必须应用去模糊滤波器作为预处理,以补偿 PSF 和 RTM 在粘声介质中的图像振幅衰减。与不使用去模糊滤波器的传统 Q-IDLSRTM 方法相比,经过预处理的 PSF 和 RTM 图像可以帮助我们构建一个难度较低的图像域逆问题,从而提高图像质量和收敛速度。第二个关键点是,我们可以在反射图像上施加 L1 正则约束和总变异正则化,以稳定拟失真反问题的求解。多个二维和三维实验证明,与传统的 Q-IDLSRTM 和声学 IDLSRTM 方法相比,所开发的方法能在振幅保真度和空间分辨率方面获得更好的成像质量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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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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