On the basis of perturbation theory for a general horizontal homogeneous weakly anisotropic media, we consider the quartic coefficients in equations 1 and 2
to be (Farra et al., 2016; Grechka and Pech, 2006)
and
denotes the P-wave velocity in the chosen isotropic background. These expressions are appropriate for horizontal homogeneous weakly anisotropic media of any symmetry. A more general form form dipping layer is also discussed by Grechka and Pech (2006). In the specific case of orthorhombic media, the general quartic coefficients (equation A-1) can be simplified to
(24)
where
is given in equation 13. Therefore, the resulting moveout approximation takes the form of
without the long-offset normalization, which corresponds to the choice of
,
, and
from equation 2. The additional long-offset normalization factor can be included based on the same scheme as in equation 10 with
(28)
As a result, we obtain the same expression of the moveout approximation in equation 12 by Xu et al. (2005) in the main text.
3D generalized nonhyperboloidal moveout approximation