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When the migration velocity is correct and the image is focused at zero subsurface offset, the
transformation to angle domain does not change the depth of the image point (), and
the reflections are imaged at the same depth for all aperture angles
(). In contrast,
when the reflections are not focused at zero offset, the transformation to the angle-domain
maps the events at different depths for each different angle. The variability of the depth
with the aperture angle is described by the RMO function, which we want to measure and
quantify as a function of the perturbation in anisotropic parameters encountered along the
propagation paths. Below, we briefly present the approach proposed in (3), which
consists in approximating the RMO function by the first-order Taylor series expansion about
the correct migration velocity.
We use the same notation as in
(3): the
VTI velocity function parameterization is
, which is equivalent to Thomsen's
parameterization .VV is the velocity of a vertical ray, VH
is the velocity of a horizontal ray ()and VN is the NMO velocity ().
We define the perturbations as a three-component vector =
, where each component is a multiplicative factor
for each migration velocity. It generates a perturbed velocity field,
defined by .
From the analytic expression of the impulse response (derived from figure 1) and some
geometric interpretation of the transformation to the angle domain, the first-order derivatives
of the imaging depth in the angle domain with respect to perturbations in the anisotropic
parameters can be written as follows (7):
| |
(3) |
where is the phase aperture angle,
is the group aperture angle, is
the arctan of the offset dip, Ss and Sr are the slowness along
the source and receiver rays.
Similarly, since residual moveout is defined as the difference between the reflector
movement at finite angle and the reflector movement at normal incidence z0,
from equation 3, we can express the first-order derivatives of the residual moveout with
respect to perturbations in the anisotropic parameters:
| |
(4) |
The residual moveout is eventually approximated by the first-order Taylor series
expansion about the correct migration velocity (). The linearized expression is the
following:
| |
(5) |
Next: Formulation of the estimation
Up: Anisotropic parameter estimation from
Previous: Computation of ADCIGs
Stanford Exploration Project
1/16/2007