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 | 3D shot-profile migration in ellipsoidal coordinates |  |
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Our main motivation for exploring alternative 3D imaging geometries is
to facilitate the propagation of overturning events in all directions.
While this study suggests this goal is achievable, we recognize that
imaging overturning events is likely to be of greater significance in
situations where: i) the illumination from
downgoing waves is minimal (i.e. salt body shadow zones); and ii) the
seismic data acquisition enables the recording of these
events (i.e. wide apertures and long recording times). Currently,
SEP has neither a demonstrative wide-azimuth data set (with an
isotropic velocity model) for testing purposes nor the computational
power to do so. However, the ellipsoidal coordinate shot-profile
algorithm will, hopefully, be tested on an appropriate data set using
an industrial-sized cluster.
Another issue warranting mention is the additional computational
overhead associated with ellipsoidal coordinate shot-profile
migration. Below is a short list discussing 3D migration issues in
ellipsoidal (ECC) and Cartesian (CCC) coordinate systems:
- Both the inline and crossline migration aperture could be
reduced in an ECC because, unlike in a CCC, an ECC
spreads out naturally and increases the effective aperture.
(Sufficient volume sampling is still required to obtain a good
image.)
- Imaging in non-Cartesian coordinate systems require two
additional full-volume interpolations, one each between the
corresponding velocity models and image spaces. While the former
interpolation is easily parallelized, the later requires spraying
each ECC image point to a neighborhood of CCC points. This remains
difficult to parallelize efficiently, except by expanding the image
volume by a factor equal to the number of threads used for interpolation.
- Migration costs can be lowered, perhaps by an order of
magnitude, by imaging neighboring shot profiles in the same ECC
system.
- Because the ECC and CCC originate on the same initial surficial plane, no
wavefield injection is required. However, the sampling of the two
initial surfaces is different and requires an initial interpolation.
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 | 3D shot-profile migration in ellipsoidal coordinates |  |
![[pdf]](icons/pdf.png) |
Next: Conclusions
Up: Shragge and Shan: Ellipsoidal
Previous: Impulse Response Tests
2009-04-13