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During later stages there will be some comparison of any
modelling results (including the three components of displacement)
to real three-component seismic data. This could be
either purely surface or VSP, over known geology, with
some drill-core constraints and ideally known
elasticity matrices of the rock layers. Such
data I hope would be provided by a supporting
company of The Geomechanics Project.
The analysis of the equations (5)
by FIO methods in itself, without necessarily finding a solution,
may form a portion of my thesis. However,
I do plan also to find solutions. As noted above, such findings
may be achieved through some analytic reduction followed by completion
with numerics. I would compare such
solutions to a least one real-data test case and at least one
full numerical-solution test case. It should prove true that
subtleties of physical phenomena will be better accounted for by
the more complicated mathematics applied to the
equations of motion than by simpler methods such as ray-theory
solutions of the eikonal and transport equations.
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David Dalton
2004-04-20