1887
Volume 22, Issue 2
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

The standard common-midpoint (CMP) stack procedure becomes questionable as soon as varying reflector dips at about the same two-way time (TWT) are involved. There are several ways to handle that problem ranging from pre stack migration to dip moveout (DMO). This paper presents a new alternative which employs the same physical model of the medium that is in common use for migration: scatterers embedded in a known reference velocity field. Provided that backscattering can be described by the (first) Born approximation, it is possible to derive a zero-offset trace from a CMP gather by a procedure that relies entirely on known processing steps like normal moveout (NMO) and stacking.

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/content/journals/10.1071/EG991439
1991-06-01
2026-01-17
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References

  1. Beylkin, G., (1985). ‘Imaging of discontinuities in the inverse scattering problem by inversion of a causal generalized Radon transform. J. Math. Phys., 26, 99-108.
  2. Bleistein, N., Cohen, J. K., and Hagin, F. G., (1987). ‘Two and one-half dimensional Born inversion with an arbitrary reference’. Geophysics, 52, 26-36.
  3. Deregowski, S. M. and Rocca, F. (1981), ‘Geometrical optics and wave theory of constant offset sections in layered media’. Geophys. Prosp., 29, 374-406.
  4. Wenzel, F, (1990). ‘Die Born Stapelung’, Habilitationsschrift, Universitaet Karlsruhe, F. R. Germany.
/content/journals/10.1071/EG991439
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  • Article Type: Research Article
Keyword(s): Born approximation; CMP stack; scattering theory; seismic data processing

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