5-D interpolation with wave-front attributes
5-D interpolation with wave-front attributes
Most 5-D interpolation and regularization techniques reconstruct the missing data in the frequency domain by using mathematical transforms. An alternative type of interpolation methods uses wave-front attributes, that is, quantities with a specific physical meaning like the angle of emergence and wave-front curvatures. In these attributes structural information of subsurface features like dip and strike of a reflector are included. These wave-front attributes work on 5-D data space (e.g. common-midpoint coordinates in x and y, offset, azimuth and time), leading to a 5-D interpolation technique. Since the process is based on stacking next to the interpolation a pre-stack data enhancement is achieved, improving the signal-to-noise ratio (S/N) of interpolated and recorded traces. The wave-front attributes are determined in a data-driven fashion, for example, with the Common Reflection Surface (CRS method). As one of the wave-front-attribute-based interpolation techniques, the 3-D partial CRS method was proposed to enhance the quality of 3-D pre-stack data with low S/N. In the past work on 3-D partial stacks, two potential problems were still unsolved. For high-quality wave-front attributes, we suggest a global optimization strategy instead of the so far used pragmatic search approach. In previous works, the interpolation of 3-D data was performed along a specific azimuth which is acceptable for narrow azimuth acquisition but does not exploit the potential of wide-, rich- or full-azimuth acquisitions. The conventional 3-D partial CRS method is improved in this work and we call it as a wave-front-attribute-based 5-D interpolation (5-D WABI) as the two problems mentioned above are addressed. Data examples demonstrate the improved performance by the 5-D WABI method when compared with the conventional 3-D partial CRS approach. A comparison of the rank-reduction-based 5-D seismic interpolation technique with the proposed 5-DWABI method is given. The comparison reveals that there are significant advantages for steep dipping events using the 5-D WABI method when compared to the rank-reduction-based 5-D interpolation technique. Diffraction tails substantially benefit from this improved performance of the partial CRS stacking approach while the CPU time is comparable to the CPU time consumed by the rank-reduction-based method.
Body waves, Theoretical seismology, Wave propagation, Wave scattering and diffraction
897-919
Xie, Yujiang
77c46c7b-1aa6-4534-bca1-8c6a3dd40705
Gajewski, Dirk
9e5050b8-d167-48bc-8784-921b84e87ca0
1 November 2017
Xie, Yujiang
77c46c7b-1aa6-4534-bca1-8c6a3dd40705
Gajewski, Dirk
9e5050b8-d167-48bc-8784-921b84e87ca0
Xie, Yujiang and Gajewski, Dirk
(2017)
5-D interpolation with wave-front attributes.
Geophysical Journal International, 211 (2), .
(doi:10.1093/gji/ggx334).
Abstract
Most 5-D interpolation and regularization techniques reconstruct the missing data in the frequency domain by using mathematical transforms. An alternative type of interpolation methods uses wave-front attributes, that is, quantities with a specific physical meaning like the angle of emergence and wave-front curvatures. In these attributes structural information of subsurface features like dip and strike of a reflector are included. These wave-front attributes work on 5-D data space (e.g. common-midpoint coordinates in x and y, offset, azimuth and time), leading to a 5-D interpolation technique. Since the process is based on stacking next to the interpolation a pre-stack data enhancement is achieved, improving the signal-to-noise ratio (S/N) of interpolated and recorded traces. The wave-front attributes are determined in a data-driven fashion, for example, with the Common Reflection Surface (CRS method). As one of the wave-front-attribute-based interpolation techniques, the 3-D partial CRS method was proposed to enhance the quality of 3-D pre-stack data with low S/N. In the past work on 3-D partial stacks, two potential problems were still unsolved. For high-quality wave-front attributes, we suggest a global optimization strategy instead of the so far used pragmatic search approach. In previous works, the interpolation of 3-D data was performed along a specific azimuth which is acceptable for narrow azimuth acquisition but does not exploit the potential of wide-, rich- or full-azimuth acquisitions. The conventional 3-D partial CRS method is improved in this work and we call it as a wave-front-attribute-based 5-D interpolation (5-D WABI) as the two problems mentioned above are addressed. Data examples demonstrate the improved performance by the 5-D WABI method when compared with the conventional 3-D partial CRS approach. A comparison of the rank-reduction-based 5-D seismic interpolation technique with the proposed 5-DWABI method is given. The comparison reveals that there are significant advantages for steep dipping events using the 5-D WABI method when compared to the rank-reduction-based 5-D interpolation technique. Diffraction tails substantially benefit from this improved performance of the partial CRS stacking approach while the CPU time is comparable to the CPU time consumed by the rank-reduction-based method.
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More information
Accepted/In Press date: 1 August 2017
Published date: 1 November 2017
Additional Information:
Funding Information:
We thank the Applied Seismics Group in Hamburg for continuous discussion. We thank the sponsors of the Wave Inversion Technology (WIT) Consortium for technical support and SEG for providing the data. Y. Xie would like to thank Ransheng Chen (China JK Institute of Engineering Investigation and Design) to discuss the DE algorithm in actual implementation and also thanks the China Scholarship Council (CSC) for partially funding this work. We are grateful to the editors and reviewers for their comments and suggestions.
Publisher Copyright:
© The Authors 2017.
Keywords:
Body waves, Theoretical seismology, Wave propagation, Wave scattering and diffraction
Identifiers
Local EPrints ID: 474734
URI: http://eprints.soton.ac.uk/id/eprint/474734
ISSN: 0956-540X
PURE UUID: 1b8b6cb0-8279-4f33-80b1-eac40458300d
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Date deposited: 02 Mar 2023 17:37
Last modified: 17 Mar 2024 13:04
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Author:
Dirk Gajewski
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