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| Measuring image focusing for velocity analysis | |
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Next: Image curvature and residual
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In presence of point diffractors,
the semblance functional defined in expression 1
yields unbiased estimates of the velocity parameter .
However, when the curvature is finite, the dip components
would not be aligned for the correct value of and the estimates
would be biased.
To remove this bias we can correct the dip-decomposed images
for the presence of curvature.
In Appendix A I show the simple derivation of this
correction that amounts to the following spatial shift,
, along
the normal to the structural dip,
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(A-2) |
where is the local radius of curvature,
is the local dip and is the vector
normal to the dip and directed towards increasing depth.
Notice that the application of this correction
requires the estimation of local dip
.
To estimate the local dips,
I used the Seplib program Sdip that implements
a variant of the algorithms described by Fomel (2002).
Expression 2 can be used directly to create an
ensemble to dip-decomposed images that are corrected for the local
curvature
.
The image-focusing semblance can be computed
on these images as:
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(A-3) |
However, the application of correction 2
can be quite expensive unless it is performed together with residual migration.
Furthermore, precomputing the curvature-corrected images
would further increase
the dimensionality of the image space, creating obvious problems
for handling the resulting bulky data sets.
Fortunately, when the ensemble of
the dip-decomposed images
are the result of residual prestack migration,
the curvature correction can be efficiently
computed during the evaluation of the semblance
functional 3.
Correction 2 becomes a simple interpolation
along the residual velocity parameter , as a function
of the aperture angles and dips.
To derive the interpolating function,
I first recall the expression of residual migration
in Biondi (2008a):
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(A-4) |
where
is the normal shift applied by residual migration,
is the value of after residual migration and
is the value of before residual migration,
which is usually set to be equal to one.
The parameter is a constant that is equal to the depth
for which the residual migration in 4 is exact.
Equating the normal shift in 4 with the normal shift
in 2 and solving for
we obtain
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(A-5) |
In this case,
is the of the images from which the data are interpolated from,
and
is the of the images after correction; that is,
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(A-6) |
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| Measuring image focusing for velocity analysis | |
|
Next: Image curvature and residual
Up: Unbiased measure of image
Previous: Unbiased measure of image
2009-05-05