TRUE-AMPLITUDE SEISMIC IMAGING

Protasov M.I.; Cheverda V.A.

dc.contributor.author	Protasov M.I.
dc.contributor.author	Cheverda V.A.
dc.date.accessioned	2024-11-09T08:38:22Z
dc.date.available	2024-11-09T08:38:22Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13529076
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 3, 441-445
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46449
dc.description.abstract	The objective of our paper is to compute images of reflecting–scattering elements in the investigated geological medium for a given velocity model, i.e., for a model that describes the traveltime of waves with a sufficient degree of accuracy. At present, many approaches exist for computing wave images. All of them can be divided into two main (kinematic and dynamic) families. In our work, we shall deal with the dynamic approach. We shall be interested in the procedures for computing the images in true amplitudes, i.e., in amplitudes whose realizations are used to compute images free of the influence of the overlying strata and the system of perturbation and recording (illumination conditions).
dc.title	TRUE-AMPLITUDE SEISMIC IMAGING
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06030214