BAYESIAN ESTIMATION IN SEISMIC INVERSION. PART I: PRINCIPLES<sup>1</sup>

A. J. W. Duijndam

Geophysical Prospecting · 1988 · 195 citations · 24 references

Concepts

TL;DR

The Bayesian approach, fundamentally probabilistic, is applicable to all inverse problems and can be derived within classical probability theory (e.g., Tarantola and Valette). This paper reviews Bayesian parameter estimation and discusses its full resolution and uncertainty analysis in Part II. The method combines data with prior information to produce an a posteriori probability density function, from which parameter estimates are obtained by maximizing this distribution. Depending on noise type and prior information, procedures such as least‑squares or l1‑norm inversion yield unique, stable estimates, with instability only in highly pathological cases.

Abstract

ABSTRACT This paper gives a review of Bayesian parameter estimation. The Bayesian approach is fundamental and applicable to all kinds of inverse problems. Its basic formulation is probabilistic. Information from data is combined with a priori information on model parameters. The result is called the a posteriori probability density function and it is the solution to the inverse problem. In practice an estimate of the parameters is obtained by taking its maximum. Well‐known estimation procedures like least‐squares inversion or l 1 norm inversion result, depending on the type of noise and a priori information given. Due to the a priori information the maximum will be unique and the estimation procedures will be stable except (in theory) for the most pathological problems which are very unlikely to occur in practice. The approach of Tarantola and Valette can be derived within classical probability theory. The Bayesian approach allows a full resolution and uncertainty analysis which is discussed in Part II of the paper.

References

24