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Deconvolution with the l 1 norm

Taylor, H. L., Banks, S. C., McCoy, J. F.·1979·Geophysics

Abstract

Given a wavelet w and a noisy trace t = s * w + n, an approximation s of the spike train s can be obtained using the l 1 norm. This extraction has the advantage of preserving isolated spikes in s. On some types of data the spike train s can represent s as a sparse series of spikes, which may be sampled at a rate higher than the sample rate of the data trace t. The extracted spike train s may be qualitatively much different than those commonly extracted using the l 2 norm.The l 1 norm can also be used to extract a wavelet w from a trace t when a spike train s is known. This wavelet extraction can be constrained to give a smooth wavelet which integrates to zero and goes to zero at the ends.Given a trace t and an initial approximation for either s or w, it is possible to alternately extract spike trains and wavelets to improve the representation of trace t.Although special algorithms have been developed to solve l 1 problems, all of the calculations can be performed using a general linear programming system. Proper weighting procedures allow these methods to be used on ungained data.

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Metadata

Authors
Taylor, H. L., Banks, S. C., & McCoy, J. F.
Venue
Geophysics
Published
1979-01-01
Volume
44
Issue
1
Pages
39-52
ISSN
  • 0016-8033 (ISSN-L)
  • 1942-2156
OpenAlex
W2085842701
Cited by
436
References
0
FWCI
2.18
Type
journal article
Language
en
Open access
closed

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