Next: INTERPOLATION WITH SPATIAL PREDICTORS
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The really interesting issue is whether this method
works for data that is inadequately sampled in x,
i.e. when the spectrum of the underlying wavefield is
nonvanishing above the spatial Nyquist frequency of the sampled field.
I think it might work
if the spectrum has energy below spatial Nyquist as well as above.
The method that chooses p
might be insensitive to
signal above spatial Nyquist
because temporal frequencies
below Nyquist are all agreed on the same p
whereas temporal frequencies above the spatial Nyquist
fit different values of p.
After the wavefields are interpolated,
perhaps by repetitive interlacing,
the question of aliasing no longer arises.
So, if you can bootstrap yourself up to the right solution,
I think you will stay there.
Next: INTERPOLATION WITH SPATIAL PREDICTORS
Up: INTERPOLATION WITH P.D.E. DIP
Previous: PDE to reject two
Stanford Exploration Project
1/13/1998