A depth-variant seismic wavelet extraction method for basis pursuit inversion with impedance trend constraint

IF 3 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Geophysics Pub Date : 2024-02-23 DOI:10.1190/geo2023-0255.1
R. Cai, Chengyu Sun, Zhen’an Yao, Shizhong Li
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引用次数: 0

Abstract

The seismic images produced by pre-stack depth migration show more accurate subsurface structures than time images, resulting in a growing need for depth-domain inversion. However, due to the strong non-stationarity exhibited by depth-domain seismic data, time-domain inversion methods based on the convolutional model cannot be directly applied in the depth domain. To address this issue, we have developed a method for extracting a depth-variant seismic wavelet, which is then combined with a non-stationary convolutional model to enable direct inversion of the depth-domain acoustic impedance. First, we extend the Morlet wavelet to the depth domain and propose an orthogonal matching pursuit spectral decomposition method using the depth-domain Morlet wavelet. We then investigate the waveforms and wavenumber spectra similarities between the depth-domain Morlet wavelet and depth-domain Ricker wavelet and extract depth-variant Ricker wavelets from the depth-wavenumber spectrum. We add a depth-domain impedance trend constraint to the conventional basis pursuit inversion to enhance the lateral continuity of the inversion results. Then, we attain direct inversion of the depth-domain acoustic impedance. Tests of synthetic and field data demonstrate that the proposed method achieves high-accuracy inversion results while maintaining high computational efficiency, highlighting our approach's effectiveness and strong reservoir characterization potential.
基于阻抗趋势约束的基序反演深度变异地震小波提取方法
叠前深度迁移产生的地震图像比时间图像能显示更精确的地下结构,因此对深度域反演的需求日益增长。然而,由于深度域地震数据表现出很强的非稳态性,基于卷积模型的时域反演方法无法直接应用于深度域。为解决这一问题,我们开发了一种提取深度变异地震小波的方法,然后将其与非稳态卷积模型相结合,从而实现深度域声阻抗的直接反演。首先,我们将 Morlet 小波扩展到深度域,并提出了一种使用深度域 Morlet 小波的正交匹配追寻频谱分解方法。然后,我们研究了深度域 Morlet 小波和深度域 Ricker 小波之间的波形和波谱相似性,并从深度波谱中提取了深度变异 Ricker 小波。我们在传统的基序反演中加入了深域阻抗趋势约束,以增强反演结果的横向连续性。然后,我们实现了深度域声阻抗的直接反演。对合成数据和现场数据的测试表明,所提出的方法既能获得高精度的反演结果,又能保持较高的计算效率,凸显了我们方法的有效性和强大的储层表征潜力。
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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