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Abstract

A.purely empirical approach that has been used to the seismic and well data is to apply a set of trial phase rotations to the seismic data. With certain provisos on data requirements and available bandwidth such an approach can be automated by using a maximum kurtosis criterion to select the desired phase correction (White, 1986). Whilst there is no apparent theoretical reason why phase rotations alone should be sufficient to zero-phase processed seismic data, this very simple procedure can be surprisingly effective in many cases. In this paper we explore the physical justification for such a one-parameter phase-scan in terms of the nature of the error arising out of conventional deconvolution processing. We derive another set of one-parameter phase filters that are physically more meaningful and also allow zero-phasing of marine data through kurtosis maximization.

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/content/papers/10.3997/2214-4609.201409775
1994-06-10
2024-04-19
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