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Substituting the theoretical interval velocity
from equation (40)
into the definition of
RMS velocity
(equation (25))
yields:
|  |
(47) |
| (48) |
Thus the desired expression for RMS velocity
as a function of traveltime depth is:
|  |
(49) |
For small values of
,this can be approximated as
|  |
(50) |
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Stanford Exploration Project
12/26/2000