Results: Models
As described in the method section, we
perform a multi-step inversion procedure. The final result is a model
of three-dimensional shear velocity perturbations. The 3-D model uses
cells for the lateral parameterization and layers for the vertical
parameterization. The layers span the depth ranges:
- 25-100 km
- 100-200 km
- 200-300 km
Viewing all three layers together is a nice way
to see the changes, as a function of depth, in the model.
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Questions? woodward@asl.cr.usgs.gov