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The Geomechanics Project has so far focused on ray trajectories
and traveltimes within seismic ray theory rather than displacement
amplitudes in the context of the transport equation or
otherwise. While three-component displacement modelling
is only one aspect of my research, it should complement
other studies within the Geomechanics Project and extend
recent results in the literature on amplitude modelling
in fully elastic inhomogeneous media.
The proposed application of FIOs
to analyzing the equations of motion should extend
the results of previous analyses of the transport equation.
As well, it is a new approach that may reveal subtleties of modelling.
With comparison to standard method of characteristics and
principal symbol variant and to full numerical methods for
at least one test case and real data over known geology
for at least one test case it would form a substantial
body of work sufficient for a Ph.D. This research
ought to result in some primary publications and conference presentations
during the degree years and immediately following degree completion.
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David Dalton
2004-04-20