Generally, advanced macro model estimation techniques need an initial macro velocity model of the subsurface to start with. A conventional way of building such a model is by interpolating the stacking velocity analyses carried out at a number of locations along the seismic line. An alternative way of estimating the initial velocity model based on the parabolic Radon transform is presented here. The increased resolution of the least squares parabolic Radon transform is the key element of the proposed technique. Also it is shown that the same transform domain can be used as the velocity stack domain and an improved version of the stack (equivalent to the conventional velocity stack) can be obtained by picking events in the high resolution transform domain.
Original languageEnglish
Title of host publication1994 SEG Annual Meeting
PublisherSociety of Exploration Geophysicists
Pages1473-1476
Publication statusPublished - 1994
EventSEG 1994: 1994 Society of Exploration Geophysicists Annual Meeting - Los Angeles, United States
Duration: 23 Oct 199428 Oct 1994

Conference

ConferenceSEG 1994: 1994 Society of Exploration Geophysicists Annual Meeting
Abbreviated titleSEG 1994
CountryUnited States
CityLos Angeles
Period23/10/9428/10/94

ID: 47686883