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Abstract

Summary

This case study demonstrates a practical application of a geologically conditioned seismic amplitude inversion workflow. The applied method is based on a quantitative parameterization of a-priori geological knowledge where the diversity of sedimentary environments is described by a few statistically independent parameters (G-Factors). Interpolated values of G-Factors were used to estimate facies a-priori probabilities in the interwell space. The structural framework of the target interval was described with a probabilistic approach: for each elementary stratigraphic unit a probability cube was generated, which allowed taking into account kinematical uncertainties of seismic interpretation. Then a-priori lithotype probabilities as well as a-priori petrophysical properties distributions were estimated for each cell of the 3D grid. The integrated a-priori model was used to build a background model for seismic amplitude inversion as well as for quantitative interpretation of the inversion results.

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/content/papers/10.3997/2214-4609.201901299
2019-06-03
2024-04-26
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References

  1. Davison, M.L.
    [1983] Multidimensional scaling. John Wiley & Sons, New York.
    [Google Scholar]
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