📄 refrealazihti.par.main
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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
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