Surface-related multiple attenuation with least-squares multidimensional deconvolution for P and S reflections in OBC/OBN data

被引:0
作者
Yang, JinRong [1 ]
Cheng, JiuBing [1 ]
Wang, TengFei [1 ]
Zhu, Feng [1 ,2 ]
Wu, SiHai [1 ,3 ]
机构
[1] Tongji Univ, State Key Lab Marine Geol, Shanghai 200092, Peoples R China
[2] Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN USA
[3] Sinopec Geophys Res Inst, Nanjing 211103, Peoples R China
来源
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION | 2025年 / 68卷 / 04期
关键词
Surface-related multiple; Ocean bottom observation; Multicomponent; Wavefield decomposition; Converted wave; Least-squares; Multidimensional deconvolution; Up/down deconvolution; REVERSE TIME MIGRATION; WAVE-FIELD DECOMPOSITION; VIRTUAL SOURCE METHOD; SEISMIC DATA; ADAPTIVE DECOMPOSITION; SCATTERING SERIES; ELIMINATION; SUPPRESSION; INVERSION; AVO;
D O I
10.6038/cjg2024S0533
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
Due to the presence of the interfaces at the ocean surface and bottom, the subsurface reflected/scattered waves are strongly influenced by surface-related multiples, posing a great challenge to the processing of multicomponent ocean-bottom seismic data, especially in velocity model building and seismic migration. Conventional demultiple methods for streamer data are not only challenged in processing ocean-bottom data, buthard to handle converted waves. Based on data-driven redatuming, we propose an regularized least-squaresinversion to solve the problem of up/down multidimensional deconvolution (MDD), according to the multidimensional convolution relationship among the up/down-going P or S waves and the impulsive reflections, so that the effectsof water layer and free surface on PP and PS reflections are eliminated. Synthetic data examples have illustratedthe mechanism of least-squares up/down MDD method, and demonstrated its precision advantage overconventional up/down deconvolution (UDD). These experiments have demonstrated the potential of the proposedapproach to improve imaging of the PP and PS reflections through attenuating the surface-related multiples,especially in the presence of complex geologic structures in shallow water.
引用
收藏
页码:1457 / 1471
页数:15
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