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In the case of VTI, based on Harlan (1995)
and later rediscovered by Etgen and Brandsberg-Dahl (2009), Crawley et al. (2010),
Pestana et al. (2012) and Zhan et al. (2012)
where they started from the exact phase velocity expression for VTI media,
equation 4.3 becomes
 |
(44) |
Here,
and
represent the normal moveout (NMO) velocity and the P-wave velocity in the horizontal direction, respectively;
and
are Thomsen's (1986) parameters.
The resulting anisotropic wave equation derived in this way is known as the
decoupled or pure P-wave equation, where the P-wave and shear-wave are separated and
there is no spurious shear-wave artifacts in the P-wave simulation.
Ge Zhan
2013-07-09