Translations:Attenuation/16/en
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Schuster (2005)[1] derived an interferometric form of Fermat’s principle that helps us to perform high-resolution estimation of the velocity distribution among deep interfaces. He used Fermat’s interferometric principle to redatum the surface sources and receivers to interface A kinematically. The velocity model above interface A does not need to be known, so the distorting effects of the overburden and statics are eliminated by his target-oriented approach.
- ↑ Schuster, G. T., 2005, Fermat’s interferometric principle for target-oriented traveltime tomography: Geophysics, 70, no. 4, U47–U50.