Nonminimum phase deconvolution in the log domain: A sparse inversion approach

Author:

Guitton Antoine1,Claerbout Jon2

Affiliation:

1. Geo Imaging Solutions, Inc., San Mateo, California, USA..

2. Stanford University, Stanford, California, USA..

Abstract

Being disturbed by the discrepancy between the Ricker wavelet and minimum phase wavelets, we wondered if a sparseness criterion could get us deconvolved data with the event polarity being more clearly evident. Five data sets found it does. The sparseness criterion we used is a hyperbolic penalty function. It ranged from [Formula: see text] at small residuals to [Formula: see text] at large residuals. The main pitfall was that introducing negative filter lags introduced a null space (obviously so for Gaussian data). The null space demanded a regularization. We found a formulation in the domain of the Fourier transform of a log spectrum, in which a Ricker-style regularization appeared. Curiously, this regularization eliminated the leg jumps. A quasi-Newton solver was faster than that of our earlier work, a combination of conjugate directions with a Newton solver.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference16 articles.

1. Deconvolution of marine seismic data using the l1 norm

2. Claerbout, J., and S. Fomel, 2014, Geophysical image estimating by example, www.lulu.com, accessed 18 April 2015.

3. Ricker-compliant deconvolution

4. Fowler, P. J., 1988, Seismic velocity estimation using prestack time migration: Ph.D. thesis, Stanford University.

5. Homomorphic deconvolution

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