THE HYPERBOLIC RADON TRANSFORM AND SOME OF ITS APPLICATION IN SEISMIC DATA PROCESSING

Suprajitno Munadi

Abstract


The Radon transform has been used in exploration seismology for a decade. It consists of stacking seismic traces along a line of constant ray parameter p. this transform is used to map seismic data from time distance space into tau-p space, where tau is the intercept time.


Keywords


Hyperbolic Radon, Seismic, Exploration Seismology

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References


Bazelaire, E., Desaunay, S. and Viallix, J.R., 1991, “The hyperbolic Radon transform”, European Association of Exploration Geophysicists, 53rd Annual Meeting, Florence.

Bessonova, E.N., Fishman, V.M., Ryaboyi, V.Z., and Sitnikova, G.A., 1974, “The tau method for inversion of travel time –I: deep seismic sounding data”, Geophysical Journal, 36, 377-398

Bessonova, E.N., Fishman, V.M., Ryaboyi, V.Z., and Sitnikova, G.A., 1976, “The tau method for inversion of travel time II : Earthquake data”, Geophysical Journal, 41, 87-108




DOI: https://doi.org/10.29017/SCOG.15.1.1113

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