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The theory behind the interpolation scheme presented here
could also be used to address the problem of cross-line smear
in 3-D marine surveys, discussed by Yilmaz (1987). Cable
feathering causes midpoint locations to be distributed over
the cells of a 3-D marine survey. If there is a significant
amount of cross-dip in the subsurface, this midpoint scatter
brings with it time shifts that cause a departure from
hyperbolic moveout, and a smearing of the stacked amplitudes.
Removal of the midpoint smear requires an estimate of the dip.
The algorithm described here could be used to automatically determine the
dip. Time shifts could be computed
and applied to map all midpoints to the cell center.
Next: Conclusions
Up: FIELD DATA EXAMPLE
Previous: An alternate approach -
Stanford Exploration Project
11/18/1997