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Now let us be specific about what is meant by the lens term
in the present context of before-stack migration
in the presence of lateral velocity variation.
Specializing the DSR equation to 15
angles gives
| ![\begin{displaymath}
{ \partial U \over \partial z } \eq - \ \Biggl\lbrace \ \lef...
...ial^2 \ \over \partial g^2}
\ \right] \ \Biggr\rbrace \ U \quad\end{displaymath}](img82.gif) |
(17) |
Rearranging the terms to group by behavior gives
|  |
(18) |
| (19) |
So you see the familiar type of lens term, but it has two parts,
one for shifting at the shot, and one for shifting at the geophone.
Next: The migrated time section:
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Stanford Exploration Project
10/31/1997