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The first part (Chapter
) covers the
multidimensional spectral factorization of passive seismic wavefields.
I show that calculating the 3-D spectral factorization of a passive
seismic wavefield amounts to estimating the medium's 3-D impulse
response.
Helioseismic dopplergrams provide a high-quality passive seismic
dataset that has uniquely dense spatial coverage.
This enables me to compare the solar impulse response from derived by
spectral factorization with that derived by cross-correlation.
The spectral factorization results contain significantly higher
bandwidth, both temporally and spatially.
I then show it is possible to derive active-source seismograms from
terrestrial passive seismic data by crosscorrelating and factorizing
data collected during a small passive seismic experiment conducted in
Long Beach, CA.
Next: Spectral factorization of partial
Up: Applications of multi-dimensional spectral
Previous: Applications of multi-dimensional spectral
Stanford Exploration Project
5/27/2001