The Interplay of Framelet Transform and lp Quasi-Norm to Interpolate Seismic Data

被引:1
|
作者
Pan, Xiao [1 ]
Wu, Hao [1 ]
Chen, Yingpin [2 ]
Qin, Zhiqiang [3 ]
Wen, Xiaotao [1 ]
机构
[1] Chengdu Univ Technol, Key Lab Earth Explorat & Informat Tech, Minist Educ, Chengdu, Peoples R China
[2] Minnan Normal Univ, Sch Phys & Informat Engn, Zhangzhou, Peoples R China
[3] Shandong Prov Lunan Geol & Explorat Inst, Shandong Prov Bur Geol & Mineral Resources No, Geol Brigade 2, Jining, Peoples R China
关键词
Geoscience and remote sensing; Wavelet transforms; Time-frequency analysis; Signal to noise ratio; Interpolation; Geology; Wavelet domain; Seismic data interpolation; seismic data processing; sparse transform; TRACE INTERPOLATION; RECONSTRUCTION; OFFSET;
D O I
10.1109/LGRS.2022.3227567
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
Missing traces affect the result of subsequent steps, such as migration and amplitude versus offset (AVO) analysis, which harms the understanding of the subsurface structure and hydrocarbon exploration. Framelet transform can sparsely represent seismic data and it can describe data in detail. Compared with the commonly used l(1) norm, l(p) quasi-norm has higher sparsity. In this letter, we establish a new subject with l(p) quasi-norm and framelet transform to reconstruct the seismic record. Instead of a conventional solver, we apply the alternating direction method of multiplier (ADMM) to solve the problem. Both synthetic test and field application prove that our proposed method not only gets a good result with high signal-noise-ratio (SNR) but also costs much less time than the conventional method. This indicates that the interplay of framelet transform and l(p) quasi-norm can do a good job in seismic data reconstruction.
引用
收藏
页数:5
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