Abstract:Seismic reflector interfaces in the subsurface are typically idealized as zero-order discontinuities. According to this model, the Earth's subsurface is represented by a spiky reflection coefficient sequence for which deconvolution methods have been derived. However, multiscale analysis on sedimentary basins reveals the existence of accumulation of varying-order singularities in the subsurface. Seismic traces with varying-order singularities violate most of the assumptions underlying conventional deconvolution… Show more
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