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By introducing geologic based smoothing filters into our tomography problem
we can obtain solutions that are more geologically reasonable and avoid some
of the non-linear traps that isotropic smoothers can fall into.
Further improvement is obtained by separating the velocity and reflector
position estimation problem by formulating our inversion in
(, ) space. Overall the methodology holds promise in producing
realistic velocity structures in areas of fairly complex geology.
Next: Velocity estimation: REFERENCESClapp, et
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Stanford Exploration Project
7/5/1998