Seismic trace interpolation in the f-x-ydomain - Imperial College London
per to the f-x-y domain. When the method is applied to 3-D seismic, the two spatial axes are defined by the in-line and cross-line directions in a common-offset (or zero-offset stack) cube. The method may also be applied to 2-D seismic traces for prestack data processing, where one spatial axis represents ................
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