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Volume 32 Number 5
  • E-ISSN: 1365-2478

Abstract

A

In odd‐depth structure the two‐way traveltime to each boundary is constrained to be an odd integer. The odd‐depth property of a model is exposed to possible refutation under a seismogram test. Test function is a simple transformation of a synthetic seismogram. For an odd‐depth model the test function has identically the value 1.

The testability of a synthetic seismogram over an odd‐depth structure provides a method of deterministic deconvolution. There is no need of specialized assumptions, like the minimum‐phase property, about the source wavelet. The deconvolution may be performed in the absence of the early segment of a seismogram.

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/content/journals/10.1111/j.1365-2478.1984.tb00740.x
2006-04-27
2024-04-20

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References

  1. Claerbout, J. F.1968, Synthesis of a layered medium from its acoustic transmission response, Geophysics33, 264–269.
    [Google Scholar]
  2. Koehler, F. and Taner, T.1977, The direct and inverse problems relating reflection coefficients and reflection response for horizontally layered media, Geophysics42, 1199–1206.
    [Google Scholar]
  3. Robinson, E. A. and Treitel, S.1965, Dispersive digital filters, Reviews of Geophysics4, 433–461.
    [Google Scholar]
  4. Robinson, E. A. and Treitel, S.1978, The fine structure of the normal incidence synthetic seismogram, Geophysical Journal of the Royal Astronomical Society53, 289–310.
    [Google Scholar]
  5. Szaraniec, E.1966, Méthode générale de calcul de la répartition du potentiel électrique à la surface d'un milieu à limites parallèles de division, Acta Geophysica Polonica14, 75–112.
    [Google Scholar]
  6. Szaraniec, E.1976, Fundamental functions for horizontally stratified earth, Geophysical Prospecting24, 528–548.
    [Google Scholar]
  7. Ziolkowski, A.1982, Further thoughts on Popperian geophysics—The example of deconvolution, Geophysical Prospecting30, 155–165.
    [Google Scholar]
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  • Article Type: Research Article

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