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Decon in the log domain with variable gain |
in the log spectrum of the deconvolution filter.
Given data
, the deconvolved output is
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(1) |
.
The log variables
transform the linear least squares (
) problem
to a non-linear one that requires iteration.
Losing the linearity is potentially a big loss,
but we lost that at the outset when we first realized
we needed to deal with the non-minimum phase Ricker wavelet.
We find convergence is typically quite rapid.
The source wavelet, inverse to the decon filter above, corresponds to
.
The positive lag coefficients in
correspond
to a causal minimum phase wavelet.
The negative lag coefficients correspond to an anticausal filter.
Here for the first time we introduce the complication
that seismic data is non-stationary
requiring a time variable gain
.
The deconvolved data is the residual
.
The gained residual
is ``sparsified''
(Li et al., 2012)
by minimizing
where
Our prefered penalty function
used for finding
is the hyperbolic (or hybrid) penalty function
(equation (3)).
The output
best senses sparsity when
gain is such that the typical penalty
value
is found near the transition level between
and
norms,
namely, when typical
.
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Decon in the log domain with variable gain |