1887

Abstract

In seismic interpretation, one of the most essential steps is time-to-depth conversion. Nevertheless, up to the present very crude techniques have been used for that purpose, such as vertical stretching of the time migrated horizons on basis of velocities measured from Wells .

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/content/papers/10.3997/2214-4609.201410545
1992-06-01
2020-09-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410545
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