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The same relationships can be easily adapted to heterogeneous media
Biondi (2005b) by converting the depth
errors in ADCIGs into traveltime errors that can used for tomography.
The conversion to traveltime errors is done by rewriting the chain of
partial derivatives:
| ![\begin{eqnarray}
\frac{\partial z_\gamma}{\partial t}
&=&
\frac{\partial z_\gamm...
...+S_s}{1+\Delta_{\tilde{S}}\tan\left(\alpha_x \right) \tan \gamma}.\end{eqnarray}](img63.gif) |
|
| (36) |
Next: Synthetic-data examples of RMO
Up: Anisotropic residual moveout for
Previous: RMO function with arbitrary
Stanford Exploration Project
4/6/2006