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Abstract

Today, most of seismic data interpretations are based on the automatic picking using workstations. However, the efficiency of such interpretations require the use of a zero phase signal. In order to control the zero phasing, we use the wavelet transform [1]. This technique allows us to describe the time evolution phase spectrum. In this paper, we present the theory of the method, then we analyse same synthetic models and seismic data.

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/content/papers/10.3997/2214-4609.201409485
1995-05-29
2024-04-27
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