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So far I have, as outlined in subsection 2.2 below,
applied the method of characteristics to the equations of
motion to get a long determinantal eikonal equation. In
the case of isotropy this equation reduces to the eikonal equations for P and S
waves. This result is promising, but I will have to
use numerical methods to solve the long form eikonal equation.
I have also, as described in subsection 2.3 below,
found a principal-symbol matrix determinant
eikonal equation that is one-fifth the length of the first one.
This equation also reduces to the eikonal equations for P and S
waves for the case of isotropy. I plan to review my work
for possible errors that, when corrected, would result in the
first one and second one being identical.
As well, in the last year-and-a-half I have done
some course study and literature review
related to those courses and to my thesis research.
The four courses are:
- a lecture course on seismic waves and rays
(based on Slawinski, 2003), EASC6177;
- a reading/lecture course on differential geometry (based on Arnold, 1989),
EASC6172;
- a reading/lecture course on differential geometry (based on
Schutz, 1980), EASC6913;
- a reading/lecture course
on functional analysis, Sobolev spaces, partial differential
equations, pseudo-differential operators and Fourier-integral
operators, and method of characteristics, EASC 6912.
Next: Inhomogeneity
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David Dalton
2004-04-20