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Chapter 5 describes a downward-continuation method
to migrate 3-D converted-wave data.
This downward-continuation operator
uses the stationary-phase approximation for the full
3-D prestack downward-continuation operator. This
chapter demonstrates that is feasible to extend
the existing common-azimuth downward-continuation to
handle PS data. This PS common-azimuth operator uses
two propagation velocity models for each of the
wavefields.
Finally, I test the PS-CAM operator with the results
obtained in Chapter 4 for the real
3-D OBS dataset from the Alba oil field. I
compare two images. The first image is
the result of using normal moveout plus stacking
to obtain a common-azimuth cube.
Second, the result obtained using the method developed
in Chapter 4. The comparison between these two results show that the correct
handling of irregular geometries before the migration
yields to better image results.
Next: PS imaging operators
Up: Thesis Overview
Previous: Chapter 4: PS Azimuth
Stanford Exploration Project
12/14/2006