RETRACTED: Plane-wave orthogonal polynomial transform for amplitude-preserving noise attenuation (Publication with Expression of Concern. See vol. 221, pg. 2054, 2020) (Retracted article. See vol. 222, pg. 1896, 2020)

被引:28
作者
Chen, Yangkang [1 ]
Huang, Weilin [2 ]
Zhou, Yatong [3 ]
Liu, Wei [2 ]
Zhang, Dong [4 ]
机构
[1] Zhejiang Univ, Sch Earth Sci, Hangzhou 310027, Zhejiang, Peoples R China
[2] China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing 102249, Peoples R China
[3] Hebei Univ Technol, Sch Elect & Informat Engn, Tianjin Key Lab Elect Mat & Devices, 5340 Xiping Rd, Tianjin 300401, Peoples R China
[4] Delft Univ Technol, Dept Imaging Phys, Lorentzweg 1, NL-2628 CJ Delft, Netherlands
基金
中国国家自然科学基金;
关键词
Image Processing; Seismic Noise; EMPIRICAL MODE DECOMPOSITION; SEISMIC DATA; SEISLET TRANSFORM; REDUCTION; SUPPRESSION; SEPARATION; PREDICTION; RECOVERY; SPECTRUM; DOMAIN;
D O I
10.1093/gji/ggy267
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
Amplitude-preserving data processing is an important and challenging topic in many scientific fields. The amplitude-variation details in seismic data are especially important because the amplitude variation is directly related with the subsurface wave impedance and fluid characteristics. We propose a novel seismic noise attenuation approach that is based on local plane-wave assumption of seismic events and the amplitude preserving capability of the orthogonal polynomial transform (OPT). The OPT is a way for representing spatially correlative seismic data as a superposition of polynomial basis functions, by which the random noise is distinguished from the useful energy by the high orthogonal polynomial coefficients. The seismic energy is the most correlative along the structural direction and thus the OPT is optimally performed in a flattened gather. We introduce in detail the flattening operator for creating the flattened dimension, where the OPT can be applied subsequently. The flattening operator is created by deriving a plane-wave trace continuation relation following the plane-wave equation. We demonstrate that both plane-wave trace continuation and OPT can well preserve the strong amplitude variation existing in seismic data. In order to obtain a robust slope estimation performance in the presence of noise, a robust slope estimation approach is introduced to substitute the traditional method. A group of synthetic, pre-stack and post-stack field seismic data are used to demonstrate the potential of the proposed framework in realistic applications.
引用
收藏
页码:2207 / 2223
页数:17
相关论文
共 78 条
[1]   LATERAL PREDICTION FOR NOISE ATTENUATION BY T-X AND F-X TECHNIQUES [J].
ABMA, R ;
CLAERBOUT, J .
GEOPHYSICS, 1995, 60 (06) :1887-1896
[2]  
[Anonymous], 2016, 2016 INT GEOPH C EXP
[3]  
[Anonymous], 2016, 86 ANN INT M SEG EXP, DOI DOI 10.1190/SEGAM2016-13763335.1
[4]  
[Anonymous], 2016, 78 ANN INT C EXH EAG, DOI DOI 10.3997/2214-4609.201601241
[5]  
[Anonymous], 2015, SEG TECHN PROGR EXP
[6]   Seismic Random Noise Attenuation Using Synchrosqueezed Wavelet Transform and Low-Rank Signal Matrix Approximation [J].
Anvari, Rasoul ;
Siahsar, Mohammad Amir Nazari ;
Gholtashi, Saman ;
Kahoo, Amin Roshandel ;
Mohammadi, Mokhtar .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2017, 55 (11) :6574-6581
[7]  
Asgedom EG, 2017, J SEISM EXPLOR, V26, P105
[8]   A structural rank reduction operator for removing artifacts in least-squares reverse time migration [J].
Bai, Min ;
Wu, Juan ;
Zu, Shaohuan ;
Chen, Wei .
COMPUTERS & GEOSCIENCES, 2018, 117 :9-20
[9]  
Bai M, 2018, J SEISM EXPLOR, V27, P103
[10]  
Bai M, 2018, J SEISM EXPLOR, V27, P29