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Inversion to common offset () is an accurate but
costly technique for processing irregularly sampled 3D data.
The inversion is not restricted to
zero offset models or to a particular azimuth. The model, in general,
simulates a regular common-offset experiment.
For practical 3D applications, we use a cost-effective
implementation based on a log-stretch
transformation (), after which AMO
becomes time invariant and the inversion can be split into
independent frequencies. The linear inverse problem we solve for
each frequency component can be written as:
| |
(60) |
where the vector represents the irregular input data,
represents
the modeling operator, and stands for the regularly sampled model.
Next: Diagonal weighting preconditioning
Up: Rickett, et al.: STANFORD
Previous: Estimating the data covariance
Stanford Exploration Project
7/5/1998