1887

Abstract

Summary

We consider a salt overhang model with salt body covered by sediments. The problem of modeling of the wavefield below salt body is solved with help of the cascade diffraction method. The near-front wavefield is a superposition of the feasible double-transmitted wavefield and the feasible direct wave which is a conventional direct wave corrected by the diffraction correction. We provide numerical examples which illustrate the structure of the wavefield.

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/content/papers/10.3997/2214-4609.20141260
2014-06-16
2024-04-28
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References

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