1887
Volume 27 Number 1
  • E-ISSN: 1365-2478

Abstract

A

A method is presented to derive approximate versions of the wave equation which allow finite‐difference migration for very steep dips (> 50°). It is shown that for conventional finite‐difference schemes, to the dip limitation, the maximum acceptable frequency should be specified. A finite‐difference migration technique is proposed in the frequency domain. It is derived that finite‐difference wave field extrapolation in the frequency domain consists of a convolution procedure for each frequency component, the space‐variance being defined by the variation in the velocity.

Finally it is shown that with finite‐difference migration, particle velocity data can be easily obtained from pressure data.

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/content/journals/10.1111/j.1365-2478.1979.tb00965.x
2006-04-27
2024-04-24
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References

  1. Berkhout, A. J., and van Wulfften, Palthe D. W., 1979, Migration in terms of spatial deconvolution, Geophysical Prospecting27, 261–291.
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  2. Claerbout, J. F., 1970, Coarse grid calculations of waves in inhomogeneous media with application to delineation of complicated seismic structure, Geophysics35, 407–418.
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  • Article Type: Research Article

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