1887

Abstract

The high-order spectra have been used to determine the complex phases of seismic wavelets. However, phases of high-order spectra, derived from a single seismic trace, are generally wrapped and corrupted by noise. In this paper, the wavelet is estimated us

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/content/papers/10.3997/2214-4609.201400063
2009-06-08
2024-03-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400063
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