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To handle the inherent non-stationarity of seismic data, we estimate
a filter bank of non-stationary filters using helical boundary
conditions (). This approach has been successfully
utilized by () to attenuate surface-related multiples.
We use a NLCG solver with the 1#1-norm and a standard conjugate gradient
solver with the 312#312-norm. The filter coefficients vary smoothly
across the output space thanks to a preconditioning of the problem
(). In the following results, the non-stationary filters
are 1D. We estimate the same number of coefficients per filter
with the 312#312- and 1#1-norm.
Next: Adaptive subtraction results
Up: Attenuation of internal multiples
Previous: The synthetic data
Stanford Exploration Project
6/7/2002