I. Psencik et Ja. Dellinger, Quasi-shear waves in inhomogeneous weakly anisotropic media by the quasi-isotropic approach: A model study, GEOPHYSICS, 66(1), 2001, pp. 308-319
In inhomogeneous isotropic regions, S-waves can be modeled using the ray me
thod for isotropic media. In inhomogeneous strongly anisotropic regions, th
e independently propagating qS1- and qS2-waves can similarly be modeled usi
ng the ray method for anisotropic media. The latter method does not work pr
operly in inhomogenous weakly anisotropic regions, however, where the split
qS-waves couple. The zeroth-order approximation of the quasi-isotropic (QI
) approach was designed for just such inhomogeneous weakly anisotropic medi
a, for which neither the ray method for isotropic nor anisotropic media app
lies.
We test the ranges of validity of these three methods using two simple synt
hetic models. Our results show that the QI approach more than spans the gap
between the ray methods: it can be used in isotropic regions (where it red
uces to the ray method for isotropic media), in regions of weal; anisotropy
(where the ray method for anisotropic media does not work properly), and e
ven in regions of moderately strong anisotropy tin which the qS-waves decou
ple and thus could be modeled using the ray method for anisotropic media).
A modeling program that switches between these three methods as necessary s
hould be valid for arbitrary-strength anisotropy.