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Principle of wave field extrapolation (the math)

There might be one question: where did we use the wave equation here, at all?

The answer is: in the Dispersion Formula. As I mentioned at the beginning; this is an industrial tool. It does not have any approximation, or other simplification. It is based on the only natural and real physical seismic experiment, on the shot records.

PSPI migration
PSPI migration

Sharp edges, no smiles, easy interpretation --- these are some examples of the method, what is called: phase shift migration.


Just for the better understanding; let's go back again to the wave equation, this time to the 3D version.

Wave equation

This equation can be anything. Using vector variables it will be elastic, using simple velocity, it will be skalar equation, ... etc.

The following function can be a solution, especially a plane wave, what can go any direction.

Wave equation

Small exercise: please take a piece of paper and start derivate. It is easy. Place the derivates into the wave equation. After a few simplifications you will see that the condition that our function can be a solution is, that:

Wave equation

This is nothing else but the dispersion relation. Up to this point we did not say anything special. Things start specialize, when we start working with our formulas. For example in the phase shift method we have to use wave number in z direction. To do this we must take the square root of the dispersion relation. Here we must select either the plus, or the minus part of the square root. This selection will specialize our wave equation; when we use a sign, where the z increases together with the time, we will get a downgoing wave solution; when it is opposite, it will describe and upgoing wave.

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