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We have presented an inversion algorithm for resampling unevenly spaced seismic
traces. As demonstrated with the synthetic example, the inversion process
is well constrained by using the wave equation modeling. The next step is
to study the effects of spatially aliased data on the inversion process.
It is expected that additional constraints are needed for resampling data
that are severely aliased in space.

Stanford Exploration Project

11/17/1997