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22)

Evaluation of the different terms in equation (

We show in Appendix A (equations (41) and (45))
   \begin{eqnarray}
\frac{\partial z_{\tilde{\gamma}}}{\partial L}
=
\frac{\cos ^2 ...
 ...\gamma} +
\frac{\sin \gamma}{\cos \alpha_x}
\tan \widehat{\gamma},\end{eqnarray} (23)
and
      \begin{eqnarray}
\frac{\partial L_s}{\partial S_s}
&=& 
- \frac{z_\xi}{S_s\cos(\...
 ...z_\xi}{S_r\cos(\beta_r)}=- \frac{z_\xi}{S_r\cos(\alpha_x-\gamma)}.\end{eqnarray} (24)
(25)

Using equations (23), (24) and (25), the relationship of the imaging depth in the angle domain with respect to perturbations in the anisotropic parameters can eventually be written as follows:
   \begin{eqnarray}
\frac{\partial z_{\tilde{\gamma}}}{\partial \rho_{i}}
=
-\frac{...
 ...(\alpha_x-\gamma)}
\frac{\partial S_r}{\partial \rho_{i}}
\right).\end{eqnarray} (26)

This is the fundamental equation of this section, extending the equation given in Biondi (2005a) to include dipping reflectors.

The residual moveout $\Delta z_{\rm RMO}$ is defined as the difference between the reflector movement at finite aperture angle and the reflector movement at normal incidence. The latter is given by
   \begin{eqnarray}
\left.\frac{\partial z_{\tilde{\gamma}}}{\partial \rho_{i}}\rig...
 ...ight)}
\frac{\partial S\left(\alpha_x \right)}{\partial \rho_{i}}.\end{eqnarray} (27)


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Next: RMO function with uniform Up: Anisotropic residual moveout for Previous: Geometric interpretation of the
Stanford Exploration Project
4/6/2006