Abstract
Forward and inverse wavefield continuations, introduced by G.I. Petrashen and S.A. Nahamkin, have significantly broadened the possibilities of traditional methods of seismic data processing. Multiple prediction, correction for near-surface heterogeneities, velocity-depth model construction, seismic migration, etc. in complex seismic and geological conditions require application of the wavefield continuation methods. Numerous examples presented in the paper prove the efficiency of the approach.
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