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![]() | Two-parameters residual-moveout analysis for wave-equation migration velocity analysis | ![]() |
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As a quality measurements of the gradient information,
I compute the correlation across the angle axis between
the RMO function that would be computed by picking
the maxima of the coherency spectra
and the RMO function
computed using the gradient.
For the ``Taylor'' RMO the reference
RMO function
is computed as follows:
Figure 5
compares the correlation functions
(panel a)
and
(panel b)
for the first CIG analyzed (Figure 1a).
The asterisk superimposed onto the plots of the correlation functions
is located at the maximum of the power spectrum
displayed in Figure 2a.
The coordinates
of this maximum are used to evaluate the moveout
according to equation 4.
Accurate gradient directions correspond to positive correlation
(plotted in white in the figure),
whereas potentially misleading gradient directions
correspond to negative correlation (plotted in black in the figure).
The correlation functions are mostly positive over a wide
range of parameters
,
indicating that a velocity estimation method based on these RMO functions
is likely to have good global convergence properties.
In particular,
the positive correlation functions at
indicates that the gradient computed starting from the
migrated CIG shown in Figure 2a
would be accurate, even if this CIG is far from being flat.
The correlation functions shown in Figure 5 are very similar. Therefore, the global convergence of the velocity estimation would be robust independently of whether the one-parameter or the two-parameter RMO function is used.
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CorrShift-TP
Figure 5. Correlation functions corresponding to the CIG shown in Figure 1a for: a) the ``Taylor'' two-parameter RMO function (equation 6), and b) the one-parameter RMO function (equation 7). |
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CorrShift-OP
Figure 6. Correlation functions corresponding to the CIG shown in Figure 1a for: a) the ``Orthogonal'' two-parameter RMO function (equation 11), and b) the one-parameter RMO function (equation 12). |
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Similar correlation analysis of the RMO function can be performed when
applying the ``Orthogonal'' RMO instead of the ``Taylor'' RMO.
In this case the reference
RMO function
is computed as follows:
Figure 6
compares the correlation functions
(panel a)
and
(panel b)
for the first CIG analyzed (Figure 1a).
The asterisk superimposed onto the plots of the correlation functions
is located at the maximum of the power spectrum
displayed in Figure 2b.
The coordinates
of this maximum are used to evaluate the moveout
according to equation 9.
As for the previous figure,
accurate gradient directions correspond to positive correlation
(plotted in white in the figure),
whereas potentially misleading gradient directions
correspond to negative correlation (plotted in black in the figure).
In this case the correlation functions
shown in Figure 6
are not as similar as in the previous case.
In particular, the black area around
the value
in Figure 6a
indicate that the two-parameter RMO analysis would provide
unreliable gradients.
This problem is related to the diagonal artifacts
visible in the power spectrum shown in
in Figure 2a.
These artifacts are caused by the fact that the second term
in the ``Orthogonal'' RMO function has an extremum
in the middle of the angular range,
in contrast with the other RMO functions that have
an extremum at normal-incidence.
This mid-range extremum causes spurious local maxima of the spectrum
at depths different than the normal incidence depth of the imaged reflector.
These artifacts are much weaker
when I averaged the power spectrum over a thinner depth interval (30 m)
than the one used for computing the function displayed in
Figure 6a.
The new averaging window is of thickness comparable
to the image of the reflector.
Figure 7a
shows the power spectrum obtained with this thinner averaging window,
and Figure 7b
corresponds to the two-parameters correlation function,
which is a substantial improvement with respect to the one
shown in Figure 6a.
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CorrShift-OP-narrow
Figure 7. Panel a): Two-parameter stack-power spectra resulting from RMO analysis of the CIG shown in Figure 1a obtained using a thinner averaging window (30 m) than the one used to compute the spectrum shown in Figure 2b. Panel b): Correlation function for the ``Orthogonal'' two-parameter RMO function obtained using the thinner averaging window. |
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CorrShift-TP-aniso
Figure 8. Correlation functions corresponding to the CIG shown in Figure 3a for: a) the ``Taylor'' two-parameter RMO function (equation 6), and b) the one-parameter RMO function (equation 7). |
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CorrShift-OP-aniso
Figure 9. Correlation functions corresponding to the CIG shown in Figure 3a for: a) the ``Orthogonal'' two-parameter RMO function (equation 11), and b) the one-parameter RMO function (equation 12). |
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![]() | Two-parameters residual-moveout analysis for wave-equation migration velocity analysis | ![]() |
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