Joint inversion of direct waves, primaries, and multiples for vertical cable seismic data

被引:1
|
作者
Lin, Yuzhao [1 ]
Liu, Huaishan [2 ,3 ]
Xing, Lei [2 ,3 ]
Wang, Linfei [2 ,3 ]
Zhang, Jin [2 ,3 ]
Yin, Yanxin [2 ,3 ]
Sun, Jian [1 ]
机构
[1] Ocean Univ China, Key Lab Submarine Geosci & Prospecting Tech, Minist Educ, Qingdao, Peoples R China
[2] Ocean Univ China, Key Lab Submarine Geosci & Prospecting Tech, Minist Educ, Qingdao, Peoples R China
[3] Qingdao Natl Lab Marine Sci & Technol, Evaluat & Detect Technol Lab Marine Mineral Resour, Qingdao, Peoples R China
关键词
REVERSE-TIME MIGRATION; FREE-SURFACE MULTIPLES;
D O I
10.1190/GEO2023-0475.1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
source/receiver locations. The primary and multiple wavefields are accurately reconstructed based on the reconstructed direct wavefield, and the corresponding reflectivity updates are obtained. The model-domain Hessian matrices consisting of different data are approximated by their diagonal elements to mitigate the nonuniform coverage issue, and the related covariance matrices and data-domain Hessian matrices are defined and approximated, respectively, to alleviate the calculation problem. In addition, the zero-lag correlated wavefields in the gradient are consistent with the actual wavefield propagation process, e.g., a primary wave is generated when the direct wavefield encounters reflectivity, avoiding the crosstalk. Numerical examples for synthetic models and field data illustrate that our method can accurately recover the source/receiver locations and provide high-resolution balanced-amplitude imaging results without evident crosstalk.
引用
收藏
页码:R315 / R328
页数:14
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