Seismic reflector characterization by a multiscale detection-estimation method
Seismic transitions of the subsurface are typically considered as zero-order singularities (step functions). According to this model, the conventional deconvolution problem aims at recovering the seismic reflectivity as a sparse spike train. However, recent multiscale analysis on sedimentary reco...
Main Authors: | , |
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Language: | English |
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European Association of Geoscientists & Engineers
2008
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Online Access: | http://hdl.handle.net/2429/553 |