We used the ``WEMVA works'' dataset. The starting estimate for the first WEMVA iteration was the 2000 m/s
background velocity. FEAVO effects in a slice from the angle-domain image
migrated with the background velocity are shown in the upper panel of
Figure .
We ran 10 conjugate-gradient solver iterations,
then updated the velocity model. The resulting model is shown in
the upper panel of Figure . Its peak anomalies as
departures from the background, in m/s, from left to right, are: -74, -84, +99. We migrated with this
velocity model. FEAVO effects in a slice from this image are shown in
the middle panel of Figure
. They are weaker now, but
still visible.
We performed another
WEMVA inversion loop, with 10 solver iterations, starting from the updated
velocity model. The resulting velocity model is shown in the bottom panel
of Figure . Its peak anomalies as
departures from the background, in m/s, from left to right, are: -105,
-123, +149. The angle-domain image obtained by migrating with this
new velocity model are shown in the lower panel of Figure
. The FEAVO effects are no
longer recognizable. When WEMVA's assumptions, discussed in the next
section, are satisfied and the image
perturbation can be extracted in a satisfactory manner, the inversion
process converges and the resulting velocity field is accurate enough
to reliably eliminate FEAVO effects.
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