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Each offset xj allows us to make a different estimate of
the earth model
.There are two possiblities:
i.e.
.
|  |
(3) |
|  |
(4) |
We should plot
as a function of j.
We should also plot
as a function of j
and see if we can find any higher temporal frequencies.
Next: About this document ...
Up: Claerbout: Super resolution
Previous: ROUGH V(z) MAKES TAU(t)
Stanford Exploration Project
11/11/1997