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Geometrical derivation

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
view

Consider the source and the receiver rays constrained to a slanted propagation plane as illustrated in Figure [*]-b). The plane has dip angle $\delta$.Within the propagation plane, the source ray has a dip angle $\alpha_S$ and the receiver ray a dip angle $\alpha_R$.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 $\gamma$ and the dipping angle $\alpha_n$ of the normal of the interface at the reflection point can be expressed as a function of $\alpha_S$ and $\alpha_R$:
\begin{eqnarray}
\gamma &=& \frac{\alpha_R+\alpha_S}{2} \\ \alpha_n &=& \frac{\alpha_R-\alpha_S}{2}\end{eqnarray} (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} (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} (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} (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} (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} (14)


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Next: Analytical derivation Up: REFERENCES Previous: REFERENCES
Stanford Exploration Project
7/8/2003