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An algorithm was developed to migrate the synthetic data sections.
The algorithm was adapted to handle temporal and spatial variations in
velocity. The migration of model record sections was carried out
using parameters defined in the modeling process, so that the process
was the exact inverse of that used to generate the unmigrated
sections. The migration aperture was taken across the whole seismic
section.
Next: Constant velocity sections
Up: KIRCHHOFF MIGRATION OF SYNTHETIC
Previous: Generation of synthetic seismic
Stanford Exploration Project
11/11/1997