1887

Abstract

Time-to-depth conversion has been one of the objectives of<br>seismic interpretation. There is no straightforward procedure<br>that derives a depth section from a seismic section. This is due<br>to the fact that seismic reflection times depend upon the<br>positions and shapes of the reflecting interfaces. The velocity<br>data patterns are often complex, affecting geological<br>interpretations. Depth conversion takes considerable amount<br>of an analyst's time and leaves concerns about its accuracy.<br>This uncertainty in depth conversion procedure significantly<br>contributes to pitfalls and ambiguities in depth conversion<br>velocities.

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/content/papers/10.3997/2214-4609-pdb.147.iptc11275
2007-12-04
2024-09-15
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