1887

Abstract

In prestack migration or imaging processing, estimation of a background velocity structure is a critical step. There are two main approaches to estimate seismic velocity using reflection traveltimes: one approach is traveltime tomography and the other is inversion using the coherency measure semblance.

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/content/papers/10.3997/2214-4609.201408847
1996-06-04
2024-04-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408847
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