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Figures and show the map of two anisotropy parameters, and ,
for a 2D slice of the real dataset MC311. Notice the strong anisotropic layers around the salt body.
Figure shows the image obtained by plane-wave migration, using the optimized
implicit finite-difference operator as the extrapolator. The steeply dipping sediments around the salt
below the anisotropic layers are well imaged. Figure shows the image obtained by plane-wave migration,
using an implicit isotropic operator plus a 5 point explicit anistropic correction filter Shan and Biondi (2005) as the
extrapolator. The two images are comparable, while the implicit finite-difference method is much cheaper.
Next: Conclusion
Up: Numerical examples
Previous: A synthetic dataset
Stanford Exploration Project
4/5/2006