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Many examples suggest themselves.
- We might model reflection data as a superposition
of primaries and multiples.
We might model it as a superposition of pressure waves and shear waves.
- In tomography we might model event flatness
as a superposition of shallow and deep slownesses.
The shallow and deep slownesses have wholly different
causes separated by millions of years.
They should not show crosstalk.
- The problem of segregating signal and noise
offers many examples.
We'd like to see signal containing no evident noise and vice versa.
- In time-lapse seismology we would like to see the
the image change unpolluted by the original image.
Unfortunately, the methodology proposed here does not
allow for time-shifted crosstalk.
2008-10-28