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Abstract

One of the goals of seismic data processing is to produce a section that in some way may be regarded as a subsurface cross section. The normal processing route includes NMO, CMP stacking and imaging in a post-stack migration procedure. This proces works well on areas with uniform dip. However when the stacking velocities are dip-dependent the final image will be degraded.

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/content/papers/10.3997/2214-4609.201410556
1992-06-01
2020-10-21
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410556
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