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Two promising potential future research projects would be
to demonstrate datuming
with field data for applications to land data static corrections,
and for migration in complex velocity areas.
In deep marine seismic surveys, the removal of
the water bottom multiples has long been a tricky problem.
A likely solution is to datum all the common-shot and common-receiver gathers
to a planar datum just above the water bottom,
so that water bottom multiple
travel-time period is short; conventional predictive deconvolution
(Peacock and Treital, 1979) should work well,
as in shallow water seismic surveys.
Finite-difference datuming also has potential for applications
in estimating background velocity by layer stripping procedures.
Next: ACKNOWLEDGMENTS
Up: Mo: Datuming
Previous: CONCLUSIONS
Stanford Exploration Project
11/17/1997