1887

Abstract

Additive Deconvolution is a method applied to seismic traces for obtaining first join times of signals having predefined shape. Unlike the classic deconvolution the method does not involve the computing of reverse filter operator. A seismic trace is therefore considered as a sum of weighted signals of predefined shape and noise. To obtain the coefficients of joining impulses are used the Fourier transformation and the least-squares method.

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/content/papers/10.3997/2214-4609.201403131
2006-11-26
2024-04-18
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201403131
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