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Abstract

In many seismic surveys the part of the signal following the first break has a multicyclic, 'shingled', and dispersive nature. Particulary in high--resolution seismic surveys these shingled wavetrains limit the offset-time window for observation of refiected waves and therefore are generally treated as source generated noise.

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/content/papers/10.3997/2214-4609.201407340
1997-08-09
2020-10-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407340
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