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In anisotropic wave propagation
the phase angles and velocities are different
from the group angles and velocities.
In this appendix I briefly review the concepts of phase and group
angles and velocities and the relationships between these
physical quantities.
The transformation
from phase velocity
to group velocity V
is conventionally defined as the following
Tsvankin (2001):
| ![\begin{displaymath}
V=\sqrt{\widetilde{V}^2+\left(\frac{d\widetilde{V}}{d\widetilde{\theta}}\right)},\end{displaymath}](img58.gif) |
(30) |
where
is the phase propagation angle.
The associated transformation from phase angles
to group angles
is defined
as:
| ![\begin{displaymath}
\tan \theta=
\frac
{\tan \widetilde{\theta}+ \frac{1}{\wide...
...d \widetilde{V}}{d\widetilde{\theta}} \tan \widetilde{\theta}}.\end{displaymath}](img61.gif) |
(31) |
Dellinger and Muir (1985) propose,
and heuristically motivate,
the following symmetric relations for the inverse transforms:
| ![\begin{displaymath}
\widetilde{S}=\sqrt{S^2+\left(\frac{dS}{d\theta}\right)},\end{displaymath}](img62.gif) |
(32) |
where
and S are respectively the phase slowness
and the group slowness,
and
| ![\begin{displaymath}
\tan \widetilde{\theta}=
\frac
{\tan \theta+ \frac{1}{S}\frac{d S}{d\theta}}
{1- \frac{1}{S}\frac{d S}{d\theta} \tan \theta}.\end{displaymath}](img64.gif) |
(33) |
I use the heuristic relation in equation 33
to derive some of the analytical results presented in this paper.
Furthermore, I use all the above relationships
to compute the kinematic numerical results presented
in this paper.
B
Next: Independence of depth perturbations
Up: Biondi: RMO in anisotropic
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Stanford Exploration Project
11/1/2005