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The trouble with the autocorrelation of the CSG
is that we are not accustomed to it.
We don't know how to think about it.
We would rather have the CSG itself.
This suggests spectral factorization.
In one dimension it is ancient knowledge that
spectral factorization finds us an impulse response function
of the system.
Using the helix Claerbout (1998),
in helioseismology
Rickett and Claerbout (1999a)
Rickett and Claerbout (1999b)
we found that we can recover a multidimensional causal acoustic
impulse response of the sun instead of "autocorrelation wavelets"
that helioseismologists had been getting.
Now we conjecture that we can do something similar here:
CONJECTURE:
A spectral factorization of the
(autocorrelation of the)
shot-geophone reflection data
should give us the "multidimensional impulse response" of the earth.
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There are some pitfalls with spectral factorization,
but they are fairly well understood
and they have often been overcome in the past.
Next: What if the autocorrelation
Up: AUTOCORRELATION
Previous: Need for all autocorrelations
Stanford Exploration Project
4/27/2000