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Abstract

The comparison of seismic data recorded at very different frequencies (a few hundred Hz for VSP and a few ten KHz for acoustic logging) and of dipmeter information can help for the interpretation of seismic anomalies. The VSP can have a lateral investigation of several ten or even hundred meters and a 1 to 10 meters vertical resolution. The acoustic logging used in reflected or diffracted modes has a vertical resolution of a few ten centimeters an 1 to 20 meters lateral investigation.

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/content/papers/10.3997/2214-4609.201410757
1991-05-28
2024-04-18
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410757
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