Seismic surveying and interpolation of aliased seismic traces.

摘要

In seismic surveying, spatially aliased seismic data are interpolated to produce high resolution data based on a locally planar model of reflection events using a two dimensional power diversity slant stack process that transforms the data from the t-x-y domain to t-xslope-y-slope domain, and then transforms the product to produce data using an inverse slant stack.