Low-rank Representation for Seismic Reflectivity and its Applications in Least-squares Imaging

IF 4.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Jidong Yang, Jianping Huang, Hao Zhang, Jiaxing Sun, Hejun Zhu, George McMechan
{"title":"Low-rank Representation for Seismic Reflectivity and its Applications in Least-squares Imaging","authors":"Jidong Yang,&nbsp;Jianping Huang,&nbsp;Hao Zhang,&nbsp;Jiaxing Sun,&nbsp;Hejun Zhu,&nbsp;George McMechan","doi":"10.1007/s10712-024-09828-w","DOIUrl":null,"url":null,"abstract":"<div><p>Sparse representation and inversion have been widely used in the acquisition and processing of geophysical data. In particular, the low-rank representation of seismic signals shows that they can be determined by a few elementary modes with predominantly large singular values. We review global and local low-rank representation for seismic reflectivity models and then apply it to least-squares migration (LSM) in acoustic and viscoacoustic media. In the global singular value decomposition (SVD), the elementary modes determined by singular vectors represent horizontal and vertical stratigraphic segments sorted from low to high wavenumbers, and the corresponding singular values reflect the contribution of these basic modes to form a broadband reflectivity model. In contrast, local SVD for grouped patch matrices can capture nonlocal similarity and thus accurately represent the reflectivity model with fewer ranks than the global SVD method. Taking advantage of this favorable sparsity, we introduce a local low-rank regularization into LSM to estimate subsurface reflectivity models. A two-step algorithm is developed to solve this low-rank constrained inverse problem: the first step is for least-squares data fitting and the second is for weighted nuclear-norm minimization. Numerical experiments for synthetic and field data demonstrate that the low-rank constraint outperforms conventional shaping and total-variation regularizations, and can produce high-quality reflectivity images for complicated structures and low signal-to-noise data.</p></div>","PeriodicalId":49458,"journal":{"name":"Surveys in Geophysics","volume":"45 3","pages":"845 - 886"},"PeriodicalIF":4.9000,"publicationDate":"2024-04-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s10712-024-09828-w.pdf","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Surveys in Geophysics","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s10712-024-09828-w","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

Abstract

Sparse representation and inversion have been widely used in the acquisition and processing of geophysical data. In particular, the low-rank representation of seismic signals shows that they can be determined by a few elementary modes with predominantly large singular values. We review global and local low-rank representation for seismic reflectivity models and then apply it to least-squares migration (LSM) in acoustic and viscoacoustic media. In the global singular value decomposition (SVD), the elementary modes determined by singular vectors represent horizontal and vertical stratigraphic segments sorted from low to high wavenumbers, and the corresponding singular values reflect the contribution of these basic modes to form a broadband reflectivity model. In contrast, local SVD for grouped patch matrices can capture nonlocal similarity and thus accurately represent the reflectivity model with fewer ranks than the global SVD method. Taking advantage of this favorable sparsity, we introduce a local low-rank regularization into LSM to estimate subsurface reflectivity models. A two-step algorithm is developed to solve this low-rank constrained inverse problem: the first step is for least-squares data fitting and the second is for weighted nuclear-norm minimization. Numerical experiments for synthetic and field data demonstrate that the low-rank constraint outperforms conventional shaping and total-variation regularizations, and can produce high-quality reflectivity images for complicated structures and low signal-to-noise data.

Abstract Image

地震反射率的低秩表示及其在最小二乘成像中的应用
稀疏表示和反演已广泛应用于地球物理数据的采集和处理。特别是,地震信号的低秩表示表明,地震信号可由几个主要具有大奇异值的基本模式决定。我们回顾了地震反射率模型的全局和局部低秩表示,然后将其应用于声学和粘声介质中的最小二乘迁移(LSM)。在全局奇异值分解(SVD)中,由奇异向量确定的基本模式代表了从低到高波数排序的水平和垂直地层段,相应的奇异值反映了这些基本模式对形成宽带反射率模型的贡献。相比之下,分组斑块矩阵的局部 SVD 可以捕捉非局部相似性,因此能准确地表示反射率模型,但比全局 SVD 方法的级数要少。利用这种有利的稀疏性,我们在 LSM 中引入了局部低秩正则化来估计地下反射率模型。我们开发了一种两步算法来解决这个低秩约束逆问题:第一步是最小二乘数据拟合,第二步是加权核正则最小化。对合成数据和实地数据进行的数值实验表明,低阶约束优于传统的整形和总变异正则化,并能为复杂结构和低信噪比数据生成高质量的反射率图像。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Surveys in Geophysics
Surveys in Geophysics 地学-地球化学与地球物理
CiteScore
10.00
自引率
10.90%
发文量
64
审稿时长
4.5 months
期刊介绍: Surveys in Geophysics publishes refereed review articles on the physical, chemical and biological processes occurring within the Earth, on its surface, in its atmosphere and in the near-Earth space environment, including relations with other bodies in the solar system. Observations, their interpretation, theory and modelling are covered in papers dealing with any of the Earth and space sciences.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信