1887
ASEG2004 - 17th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

An explicit, constrained operator is used for wavefield extrapolation in 3D wave equation depth migration. The migration cost and image quality benefit from its reduced number of independent coefficients, negligible numerical anisotropy, and flexibility that allows for different propagation angles and step sizes in the inline and crossline directions. In order to further reduce the computational workload we dynamically select operator lengths and extrapolation step sizes based on the wavenumber of the wave components being migrated. The phase-shifted linear interpolation that we propose for interpolating the extrapolated wavefield is suitable for the explicit migration, and significantly improves the accuracy of the result when compared with the linear interpolation typically used in implicit migrations.

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/content/journals/10.1071/ASEG2004ab121
2004-12-01
2026-01-14
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References

  1. Biondi, B. and Palacharla, G., 1995, 3D depth migration by rotated McClellan filter: Geophysical Prospecting, 43, 1005-1020.
  2. Blacquiere, G., Debeye, H. W. I, Wapenaar, C. P. A., and Berkhout, A. I, 1989, 3-D table driven migration: Geophysical Prospecting, 37, 925-958.
  3. Hale, D., 1991, 3-D depth migration via McClellan transformations: Geophysics, 56, 1778-1785.
  4. Mittet, R., 2002, Explicit 3D depth migration with a constrained operator: 72nd Annual International Meeting, SES, Salt Lake City, Expanded Abstracts, 1148-1151.
  5. Sollid, A., and Arntsen, B., 1994, Cost effective 3D one-pass depth migration: Geophysical Prospecting, 42, 755-776.
  6. Soubaras, R., 1992, Explicit 3-D migration using equiripple polynomial expansion and Laplacian synthesis: 62nd Annual Internatinal Meeting, SEG, New Orleans, Expanded Abstracts, 905-908.
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