1887

Abstract

3-D depth migration is one of the most powerful tools in seismic imaging. As in the case of time migration, this problem can be approached either in the space-time or in the wavenumber - frequency domain. The latter option is far more efficient but it cannot handle lateral variations in velocity.

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/content/papers/10.3997/2214-4609.201409232
1995-05-29
2020-11-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409232
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