1887

Abstract

To correctly image primary or multiple reflections in a heterogeneous earth, migration reigns supreme,<br>although its computational cost may be nontrivial over complex geology, in 3-D, or when a “true amplitude”<br>image is required. My earlier (Brown, 2002) technique to jointly image primaries and pegleg<br>multiples used normal moveout (NMO), because of NMO’s speed and its amplitude predictability, in<br>spite of its inability to account for nonflat geology.

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/content/papers/10.3997/2214-4609.201405724
2003-06-02
2024-03-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405724
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