Résumé
Inversion problems can be solved in different ways. One way is to define natural criteria of good recovery and build an objective function to be minimized. If, instead, we prefer a Bayesian approach, inversion can be formulated as an estimation problem where a priori information is introduced and the a posteriori distribution of the unobserved variables is maximized. When this distribution is a Gibbs distribution, these two methods are equivalent. Application to multitrace deconvolution is proposed. The introduction of a neighborhood system permits one to model the layer structure that exists in the earth and to obtain solutions that present lateral coherency. -from Author
| langue originale | Anglais |
|---|---|
| Pages (de - à) | 2008-2018 |
| Nombre de pages | 11 |
| journal | Geophysics |
| Volume | 56 |
| Numéro de publication | 12 |
| Les DOIs | |
| état | Publié - 1 janv. 1991 |
| Modification externe | Oui |
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