1. State Key Lab of Petroleum Resources and Prospecting, Beijing 102249, China;
2. CNPC Key Lab of Geophysical Exploration, China University of Petroleum (Beijing), Beijing 102249, China
Abstract:2D SRME algorithm is quite efficient, but it brings some errors in 3D multiple prediction when underground layers have a dip angle in the cross lines direction, and the adaptive subtraction is unable to compensate these errors. Therefore we develop a 3D SRME algorithm. Due to data acquisition limitation, source and receiver intervals in cross line directions are too sparse, and 2D algorithm cannot predict the exact multiples for 3D data. Assuming that a multiple contribution gather relative to a seismic trace has a shape of hyperbolas, we can conduct a sparse inversion to this corresponding multiple contribution gather to predict multiples of the trace. 3D model data tests verify the feasibility and validity of the proposed SRME algorithm.
Verschuur D J,Berkhout A J and Wapenaar C P A. Adaptive surface-related multiple elimination. Geophysics,1992,57(9):1166-1177.
[2]
Verschuur D J. Surface-Related Multiple Elimina-tion,an Inversion Approach[D]. Delft University of Technology,1991.
[3]
Ross W S,Yu Y and Gasparotto F A. Traveltime prediction and suppression of 3-D multiples. Geophysics,1999,64(1), 261-277.
[4]
Ikelle L T and Yoo S. An analysis of 2D and 3D inverse scattering multiple attenuation. SEG Technical Program Expanded Abstracts,2000,19:1973-1976.
[5]
Nekut A G. 3D surface-related multiple prediction.SEG Technical Program Expanded Abstracts,1998,17:1511-1544.
[6]
Matson K H and Corrigan D. A 2.5D method for attenuating free-surface multiples based on inverse scattering series. 32nd Annual International Meeting,Offshore Technology Conference,Proceedings,2000,12046.
[7]
Biersteker J. MAGIC:Shell's surface multiple attenuation technique. SEG Technical Program Expanded Abstracts,2001,20:1301-1304.
[8]
van Dedem E J. 3D Surface-related Multiple Prediction [D]. Delft University of Technology,2002.
[9]
Sun Y. Anti-aliasing multiple prediction beyond 2-D. SEG Technical Program Expanded Abstracts,1999,18:1338-1341.
[10]
van Dedem E J and Verschuur D J. 3D surface-related multiple prediction—An inversion approach. SEG Technical Program Expanded Abstracts,2000,19:1965-1968.
[11]
van Dedem E J and Verschuur D J. 3D surface-related multiple prediction—A sparse inversion approach. Geophysics,2005,70(3):V31-V43.
[12]
Hokstad K and Sollie R. 3D surface-related multiple elimination using parabolic sparse inversion. SEG Technical Program Expanded Abstracts,2003,22:1961-1964.
[13]
van Borselen R,Schonewille M A and Hegge R F. 3D surface-related multiple elimination:Acquisition and processing solutions. The Leading Edge,2005,24( ):260-268.
Li Hongtu,Huang Zhi,Li Zhenyong et al. 3D SRME (Surface-Related Multiple Elimination) technique and its application in deep sea seismic data processing. OGP,2009,44(S1):60-62.
Shi Ying,Wang Weihong,Li Ying et al. 3D Surface-related multiple prediction approach investigation based on wave equation. Chinese J Geophys,2013,56(6):2023-2032.
[16]
Berkhout A J. Seismic Migration,Imaging of Acoustic Energy by Wavefield Extrapolation,Part A:Theoretical Aspects. Elsevier Scientific Publ Co Inc,1982.
[17]
Sacchi M D and Ulrych T J. High-resolution velocity gathers and offset space reconstruction. Geophysics,1995,60:1169-1177.
[18]
Zwartjes P M and Duijndam A J W. Optimizing reconstruction for sparse spatial sampling. SEG Technical Program Expanded Abstracts,2000,19:2162-2165.
[19]
Shewchuk J R. An introduction to the Conjugate Gradient Method Without the Agonizing Pain. School of Computer Science,Carnegie Mellon University,1994.