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This example shows distortions that are connected with application of a wave-field
continuation operator which is not kinematically equivalent to the classical
Eiconal equation (see the next chapter).
First step: The time t0 in a true model is the same as in the
example:

Second step: If we apply 15-degree algorithm with the continuation
velocity
, then discontinuities propagate in accordance
to the Eiconal equation

(see equation (98) from Chapter 8 at
).
The solution of this equation which satisfies boundary condition
is:
![\begin{displaymath}
\tau^{(-)}(x,z)={2h_{0}\cos \phi \over v} + {\sin \phi \over...
...over v}\right) }^{2}\sin^{2}\phi \right]
{2z \over v^{\prime}}.\end{displaymath}](img436.gif)
Third step: From the condition
we find location
of the reflector image

when

The factor

so the depth distortion is very small for subhorizontal reflectors.
Next: D. CSP-depth migration in
Up: 7: GEOMETRICAL PROBLEMS OF
Previous: B. Two-layer media
Stanford Exploration Project
1/13/1998