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To derive equation (2) we will change the coordinates system
in order to find the 2-D case illustrated in Figure
-a) and
follow the derivation given in Fomel (1996).
geometry
Figure 8 a) 2-D geometry described by Sava and Fomel (2000). b) Common-azimuth formulation
of the problem. The derivation of equation (1) relies on the
definition of the problem into the propagation plane. Defined this way,
the 3-D problem becomes equivalent to the 2-D problem.
|
| ![geometry](../Gif/geometry.gif) |
Consider the source and the receiver rays constrained to a slanted
propagation plane as illustrated in Figure
-b).
The plane has dip angle
.Within the propagation plane, the source ray has a dip angle
and the receiver ray a dip angle
.We define z' as being a new vertical axis within the propagation plane:
the 3-D problem becomes a 2-D problem in this new basis.
The aperture angle
and the dipping angle
of the normal
of the interface at the reflection point can be expressed as a function
of
and
:
| ![\begin{eqnarray}
\gamma &=& \frac{\alpha_R+\alpha_S}{2} \\ \alpha_n &=& \frac{\alpha_R-\alpha_S}{2}\end{eqnarray}](img23.gif) |
(8) |
| (9) |
The offset ray parameter in the propagation plane is:
| ![\begin{eqnarray}
\frac{\partial t}{\partial h_x}
= \frac{\sin\alpha_S}{v}+\frac{\sin\alpha_R}{v}
= \frac{2}{v} \cos\alpha_n \sin\gamma\end{eqnarray}](img24.gif) |
(10) |
We can write a 2-D version of the Double Square Root (DSR) in the
propagation plane:
| ![\begin{eqnarray}
\frac{\partial t}{\partial z'}
= \frac{\cos\alpha_S}{v}+\frac{\cos\alpha_R}{v}
= \frac{2}{v} \cos\alpha_n \cos\gamma\end{eqnarray}](img25.gif) |
(11) |
The change of variable between the pseudo vertical axis z' and
the real vertical axis z is made with the
relation:
| ![\begin{displaymath}
\frac{\partial z'}{\partial z} = \cos \delta\end{displaymath}](img26.gif) |
(12) |
With equations (11) and (12) the DSR expression in the
original coordinates system becomes:
| ![\begin{displaymath}
\frac{\partial t}{\partial z} =
\frac{2}{v} \cos \alpha_n \cos \gamma \cos \delta \end{displaymath}](img27.gif) |
(13) |
The quotient of equations (10) and (13) leads to the expected
relation 2:
| ![\begin{displaymath}
\frac{\partial z}{\partial h}=
\frac{k_{h_x}}{k_z} =
\frac{\tan \gamma}{\cos \delta}\end{displaymath}](img28.gif) |
(14) |
Next: Analytical derivation
Up: REFERENCES
Previous: REFERENCES
Stanford Exploration Project
7/8/2003