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Geostatistical AVO Direct Facies Inversion

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Mathematics of Planet Earth

Part of the book series: Lecture Notes in Earth System Sciences ((LNESS))

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Abstract

In seismic reservoir characterization one aims to derive petrophysical properties of hydrocarbon reservoir conditioned to both available well-log and seismic reflection data. In this paper we present a new global pre-stack seismic AVO inversion methodology that inverts pre-stack seismic data directly for density, p-wave velocity, s-wave velocity and facies models. The retrieved subsurface models are able to reproduce the high vertical resolution of the well-log data with the spatial coverage of the seismic data. This new approach is based on an iterative genetic algorithm where the perturbation is done recurring to geostatistical simulation and co-simulation. The inverted facies model is an intrinsic part of the solution and represents the link between the elastic models (observed seismic) and the subsurface geology.

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References

  1. Shuey, R. T. (1985). A simplification of the Zoeppritz equations. Geophysics, 50(4), 609–614.

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  2. Soares, A. (2001). Direct sequential simulation and cosimulation. Mathematical Geology, 33(8), 911–926.

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  3. Horta, A., & Soares, A. (2010). Direct sequential co-simulation with joint probability distributions. Mathematical Geosciences, 42(3), 269–292.

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Correspondence to Leonardo Azevedo .

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© 2014 Springer-Verlag Berlin Heidelberg

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Azevedo, L., Correia, P., Nunes, R., Soares, A. (2014). Geostatistical AVO Direct Facies Inversion. In: Pardo-Igúzquiza, E., Guardiola-Albert, C., Heredia, J., Moreno-Merino, L., Durán, J., Vargas-Guzmán, J. (eds) Mathematics of Planet Earth. Lecture Notes in Earth System Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-32408-6_124

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