shows the slope (left), intercept (center),
and slope*intercept (right) for the migrated image
without model variability.
Note the positive, hydrocarbon indicating, anomalies circled at approximately 2.3 km.
![]() |
. The left panel shows the
slope, the center the intercept, and the right panel the
slope*intercept.
I then performed the same procedure on all of the migrated images
obtained from the various realizations (Figure
).
The left panel shows
intercept, the center panel slope, the right panel,
slope*intercept. The top shows the average of
the realizations. The center panel shows
the variance of the realizations. The bottom
panel shows the variance scaled by the inverse of the
smoothed amplitude.
What is interesting is the varying behavior at
the three zones with hydrocarbon indicators.
Figure
shows
a closeup in the zone with the hydrocarbon
indicators. The left blob `A' shows a
high variance in the AVA indicator. The
center blob `B' shows a mild variance,
and the right blob `C' shows low variance.
This would seem to indicate that
at location `C' the hydrocarbon indicator
is more valid. Without drilling
of each target a more general
conclusion cannot be drawn.
![]() |
![]() |
Conclusions I showed how AVA parameter variability can be assessed by adding a random component to our fitting goals when estimating velocity. The methodology shows promise in allowing error bars to be placed upon AVA parameter estimates.
I would like to thank Ecopetrol for the data used in this paper.