4.6 Article

Bayesian linearized AVO inversion

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GEOPHYSICS
卷 68, 期 1, 页码 185-198

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SOC EXPLORATION GEOPHYSICISTS
DOI: 10.1190/1.1543206

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A new linearized AVO inversion technique is developed in a Bayesian framework. The objective is to obtain posterior distributions for P-wave velocity, S-wave velocity, and density. Distributions for other elastic parameters can also be assessed-for example, acoustic impedance, shear impedance, and P-wave to S-wave velocity ratio. The inversion algorithm is based on the convolutional model and a linearized weak contrast approximation of the Zoeppritz equation. The solution is represented by a Gaussian posterior distribution with explicit expressions for the posterior expectation and covariance; hence, exact prediction intervals for the inverted parameters can be computed under the specified model. The explicit analytical form of the posterior distribution provides a computationally fast inversion method. Tests on synthetic data show that all inverted parameters were almost perfectly retrieved when the noise approached zero, With realistic noise levels, acoustic impedance was the best determined parameter, while the inversion provided practically no information about the density. The inversion algorithm has also been tested on a real 3-D data set from the Sleipner field. The results show good agreement with well logs, but the uncertainty is high.

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