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![]() | A robust approach to time-to-depth conversion and interval velocity estimation from time migration in the presence of lateral velocity variations | ![]() |
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vz0
Figure 12. (Top) a synthetic model and (middle) Dix velocity converted to depth. Both overlaid with image rays. (Bottom) the model perturbation for testing linearization. |
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Figure 12 shows a synthetic model borrowed from Cameron et al. (2008). The Dix inversion recovers the shallow part of the model but deteriorates quickly as geometrical spreading of image rays grows in the deeper section.
As a simple verification for the linearization process, we add a small positive velocity perturbation at location
km to the synthetic model. Comparisons between the exact and linearly predicted attributes are
illustrated in Figures 13, 14 and 15. In accordance with forward
modeling, where we solve firstly
, then
, and finally
, the linearization (see Appendix B) is carried
out following the same sequence. First, Figure 13 justifies our upwind finite-differences
implementation of the linearized eikonal equation. The positive perturbation in
in Figure 12 causes
to decrease in a narrow downwind region. Next, the area affected by the perturbation in Figure 14
is wider than that in Figure 13. It also has both positive and negative amplitudes. These phenomenon
are physical because image rays should bend in opposite directions in response to the perturbation. Finally,
effects in cost
in Figure 15 show alternating polarities and are broader in width compared to
that of
and
. They indicate a complicated dependency of
on
. Note the good agreements in
both shape and magnitude between exact and linearly predicted quantities in all three steps.
Because there is no analytical formula for Dix velocity in this model, we compute by tracing image
rays numerically in the exact model
. Also, based on Figure 12, there is no in-flow boundary other
than
. Therefore, we do not need to extend the domain as in the preceding examples. We
use the Dix-inverted model as the prior model and run the inversion. It turns out that the first linearization
update is sufficient for achieving the desired global minimum as shown in Figure 16.
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pdt
Figure 13. (Top) exact ![]() ![]() |
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pdx
Figure 14. (Top) exact ![]() ![]() |
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diffcost
Figure 15. (Top) exact ![]() ![]() |
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bgrad
Figure 16. (Top) the exact ![]() ![]() |
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![]() | A robust approach to time-to-depth conversion and interval velocity estimation from time migration in the presence of lateral velocity variations | ![]() |
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