Following the approach of Alkhalifah (1997b), an acoustic wave equation is simply derived from the eikonal equation using Fourier transformations. The addition of results in a more intriguing wave equation than the one derived by Alkhalifah. Instead of the symmetric form of the familiar Laplacian in isotropic media, two sources of unsymmetry are introduced into the new wave equation. One is caused by the unbalanced new coordinate system with one axis given in time and the other in position. The second, caused by anisotropy, is similar to that which Alkhalifah described.

Using , and
,
where *k*_{x} is the horizontal component of the wavenumber vector, is the
vertical-time-normalized component
of the wavenumber vector, and
is the angular frequency, we can transform
equation (9) to

(22) |

This equation is a fourth-order partial differential equation. Unlike, the acoustic wave equation for
VTI media
of Alkhalifah (1997b), equation (23) has odd-order derivatives caused by the unsymmetry of the
coordinate system. Setting [*v*(*z*)=0], we obtain a similar equation, with replaced by as follows:

Setting in equation (23) yields the acoustic equation for elliptically anisotropic media:

Substituting , we obtain the second-order wave equation for elliptically anisotropic media:

Rewriting equation (23) in terms of *P*(*x*,*y*,*z*,*t*) rather than *F*(*x*,*y*,*z*,*t*),
wherever possible, yields

where

Because of its second-order nature in time, equation (27) is simpler to use in a numerical implementation than equation (23). The acoustic wave equation in -domain is clearly independent of the vertical velocity when is given by equation 12 and is laterally invariant.

10/9/1997