| Summary: | Reflection moveout in azimuthally anisotropic media is not only azimuthally dependent
but it is also nonhyperbolic. As a result, the conventional hyperbolic normal moveout
(NMO) equation parameterized by the exact NMO (stacking) velocity loses accuracy
with increasing offset (i.e., spreadlength). This is true even for a single-homogeneous
azimuthally anisotropic layer. The most common azimuthally anisotropic models used
to describe fractured media are the horizontal transverse isotropy (HTI) and the orthorhombic(ORT) symmetry.
Here, we introduce an analytic representation for the quartic coefficient of the Taylor's
series expansion of the two-way traveltime for pure mode reflection (I.e., no conversion)
in arbitrary anisotropic media with arbitrary strength of anisotropy. In addition,
we present an analytic description of the long-spread (large-offset) nonhyperbolic reflection moveout (NHMO). In multilayered azimuthally anisotropic media, the NMO
(stacking) velocity and the quartic moveout coefficient can be calculated with good accuracy using the known averaging equations for VTI media. The interval NMO velocities
and the interval quartic coefficients, however, are azimuthally dependent. This allows
us to extend the nonhyperbolic moveout (NHMO) equation, originally designed for VTI
media, to more general horizontally stratified azimuthally anisotropic media. As a result, our formalism allows rather simple transition from VTI to azimuthally anisotropic
media.
Numerical examples from reflection moveout in orthorhombic media, the focus of this
paper, show that this NHMO equation accurately describes the azimuthally-dependent
P-wave reflection traveltimes, even on spreadlengths twice as large as the reflector depth.
This work provides analytic insight into the behavior of nonhyperbolic moveout, and
it has important applications in modeling and inversion of reflection moveout in azimuthally anisotropic media.
|
|---|