Cross-streamer wavefield reconstruction through wavelet domain learning

Author:

Larsen Greiner Thomas Andre1ORCID,Hlebnikov Volodya2ORCID,Lie Jan Erik3,Kolbjørnsen Odd4ORCID,Kjelsrud Evensen Andreas5,Harris Nilsen Espen3,Vinje Vetle6ORCID,Gelius Leiv-J7

Affiliation:

1. University of Oslo, Department of Geosciences, Sem Sælands vei 1, Oslo NO 0316, Norway and Lundin Norway AS, Strandveien 4, Lysaker NO 1366, Norway.(corresponding author).

2. University of Oslo, Department of Geosciences, Sem Sælands vei 1, Oslo NO 0316, Norway and CGG Lilleakerveien 6A, Box 43, Lilleaker NO 0283, Norway..

3. Lundin Norway AS, Strandveien 4, Lysaker NO 1366, Norway..

4. University of Oslo, Department of Mathematics, Moltke Moes vei 35, Oslo NO 0851, Norway and Lundin Norway AS, Lundin GeoLab, Strandveien 4, Lysaker NO 1366, Norway..

5. Lundin Norway AS, Lundin GeoLab, Strandveien 4, Lysaker NO 1366, Norway..

6. CGG, Lilleakerveien 6A, Box 43, Lilleaker NO 0283, Norway..

7. University of Oslo, Department of Geosciences, Sem Saelands vei 1, Oslo NO 0316, Norway..

Abstract

Seismic exploration in complex geologic settings and shallow geologic targets has led to a demand for higher spatial and temporal resolution in the final migrated image. Conventional marine seismic and wide-azimuth data acquisition lack near-offset coverage, which limits imaging in these settings. A new marine source-over-cable survey, with split-spread configuration, known as TopSeis, was introduced in 2017 to address the shallow-target problem. However, wavefield reconstruction in the near offsets is challenging in the shallow part of the seismic record due to the high temporal frequencies and coarse sampling that leads to severe spatial aliasing. We have investigated deep learning as a tool for the reconstruction problem, beyond spatial aliasing. Our method is based on a convolutional neural network (CNN) approach trained in the wavelet domain that is used to reconstruct the wavefield across the streamers. We determine the performance of the proposed method on broadband synthetic data and TopSeis field data from the Barents Sea. From our synthetic example, we find that the CNN can be learned in the inline direction and applied in the crossline direction, and that the approach preserves the characteristics of the geologic model in the migrated section. In addition, we compare our method to an industry-standard Fourier-based interpolation method, in which the CNN approach shows an improvement in the root-mean-square (rms) error close to a factor of two. In our field data example, we find that the approach reconstructs the wavefield across the streamers in the shot domain, and it displays promising characteristics of a reconstructed 3D wavefield.

Funder

Norges Forskningsråd

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference60 articles.

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