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This section gives an example of residual depth migration of a
post-stacked depth image. Figure
shows a synthetic slowness
model that consists of several dipping layers and a low velocity cap
over a high velocity dome. A synthetic zero-offset section is generated
from this model, as shown in Figure
. If we migrate this section
with a constant slowness, we will obtain the image displayed in
Figure
. The images of the shallow reflectors
are positioned correctly, because the interval slownesses
in these layers are close to the constant migration slowness. On the other hand,
the images of the deep reflectors are seriously mispositioned, because
the interval slownesses in these layers are considerably smaller than
the slowness used in the migration.
The low velocity cap causes the images of the bottom of the
dome to be flattened.
In order to correct the distortions of the images, I use the algorithm
described in the previous sections to calculate the residual
migration operator associated with the true slowness model and the
initial constant migration slowness. Then, I apply this operator to the
distorted image shown in Figure
. Figure
shows the output of this residual migration process. The distortion of the
images of the reflectors in position are completely corrected.
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Stanford Exploration Project
12/18/1997