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Limitation of the ray-tracing method

From the equation of de-migration (1), it is noticeable that the observed time t0 exists only if:  
 \begin{displaymath}
\left( \frac{\partial t}{\partial x} \right)_m^2 +
 \left( \frac{\partial t}{\partial y} \right)_m^2 < 
 \frac{4}{V_{rms}^2}\end{displaymath} (2)

The equation (2) above expresses the degree of limitation of the method with respect to the Vrms velocity. This means that if the dip of an initial time migrated surface overflows a certain value imposed by the value of the Vrms velocity, the de-migration process will fail.

In practice, I observed that for a dipping plane with a Vrms velocity equal to 2000m/s, this limitation problem occurs for a dip angle equal to 45 degrees.


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Next: Introducing Eikonal equation and Up: LIMITATIONS AND FUTURE WORK Previous: LIMITATIONS AND FUTURE WORK
Stanford Exploration Project
11/17/1997