App-SeismicUnixGui
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REFREALAZIHTI - REAL AZImuthal REFL/transm coeff for HTI media
refRealAziHTI [optional parameters] >coeff.data
Optional parameters:
vp1=2 p-wave velocity medium 1 (with respect to symm.axes)
vs1=1 s-wave velocity medium 1 (with respect to symm.axes)
eps1=0 epsilon medium1
delta1=0 delta medium 1
gamma1=0 gamma medium 1
rho1=2.7 density medium 1
vp2=2 p-wave velocity medium 2 (with respect to symm.axes)
vs2=1 s-wave velocity medium 2 (with respect to symm.axes)
eps2=0 epsilon medium 2
delta2=0 delta medium 2
gamma2=0 gamma medium 2
rho2=2.7 density medium 2
modei=0 incident mode is qP
=1 incident mode is qSV
=2 incident mode is SP
modet=0 scattered mode
rort=1 reflection(1) or transmission (0)
azimuth=0 azimuth with respect to x1-axis (clockwise)
fangle=0 first incidence angle
langle=45 last incidence angle
dangle=1 angle increment
iscale=0 default: angle in degrees
=1 angle-axis in rad
=2 axis horizontal slowness
=3 sin^2 of incidence angle
ibin=1 binary output
=0 Ascci output
outparfile =outpar parameter file for plotting
coeffile =coeff.data coefficient-output file
test=1 activate testing routines in code
info=0 output intermediate results
Notes:
Axes of symmetry have to coincide in both media. This code computes
all 6 REAL reflection/transmissions coefficients on the fly. However,
the set-up is such Real reflection/transmission coefficients in
HTI-media with coinciding symmetry axes.
However, the set-up is such that currently only one coefficient is
dumped into the output. This is easily changed. The solution of the
scattering problem is obtained numerically and involves the Gaussian
elimination of a 6X6 matrix. ",
Author:: Andreas Rueger, Colorado School of Mines, 02/10/95
original name of code <graebnerTIH.c>
modified, extended version of this code <refTIH3D>
Technical references:
Sebastian Geoltrain: Asymptotic solutions to direct
and inverse scattering in anisotropic elastic media;
CWP 082.
Graebner, M.; Geophysics, Vol 57, No 11:
Plane-wave reflection and transmission coefficients
for a transversely isotropic solid.
Cerveny, V., 1972, Seismic rays and ray intensities in inhomogeneous
anisotropic media: Geophys. J. R. astr. Soc., 29, 1-13.
.. and some derivations by Andreas Rueger.
If propagation is perpendicular or
parallel to the symmetry axis, the solution is analytic (see
graebner2D.c and rtRealIso.c
( run in 0.888 second using v1.01-cache-2.11-cpan-98e64b0badf )