1887

Abstract

More than the absorption in the earth layers, the processing, and more precisely the NMO correction, are responsible for the attenuation of high frequenties in seismic sections . Any improvement in the high-frequency content of the stacked sections and in the determination of the interval velocities implies, for modeling the NMO curve of the recorded reflections, a mathematical expression

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/content/papers/10.3997/2214-4609.201410503
1992-06-01
2020-09-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410503
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