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My research will focus on the mathematics of seismic wave theory in
elastic media. In particular, dealing with a three-dimensional
medium, I will study the three coupled Cauchy's equations of motion in
anisotropic inhomogeneous media using: (1) the standard method of
characteristics, (2) the principal-symbol analysis,
(3) Fourier-integral operator (FIO) theory, and (4) numerical
analysis. I have already begun and will continue to apply the method
of characteristics to the equations of motion. I have also begun to
apply principal-symbol theory (related to Fourier-integral operators)
to the equations of motion. From that I should also derive the same
characteristics. Symbols should put the equations in a framework amenable
to application of Fourier-integral operators. I will also try to
apply Fourier-integral operator theory to simple cases so that FIO
results can be tested against other known solutions. Then, I will
extend that theory to the inhomogeneous anisotropic case and ideally
show that it improves on the results of ray theory. In that general
case I expect the FIO theory will reduce the complexity of the
equations somewhat. Thus less numerical work will be required to
complete the solution than for full numerical analysis of the original
equations. That will involve some computer implementation, and
comparison to real data over known geology. The FIO modelling
results for the inhomogeneous anisotropic case can be checked by
various methods, for example, inserting the isotropic elasticity
matrix into the algorithm and checking that the solution reduces to
the isotropic solution. For at least one test case I will also check
the anisotropic inhomogeneous FIO solution against a full numerical
solution.
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David Dalton
2004-04-20