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``Picking'' is the process
of identifying dipping seismic events.
Here we will do something like picking,
but in a continuum; i.e., dips will be picked continuously
and set on a uniform mesh.
Customarily,
dip picking is done by scanning two-dimensional data along various dips.
We will see that our method,
based on the ``plane-wave destructor operator,"
does not have its resolution limited
by the spatial extent of a dip scan.
Next: The plane-wave destructor
Up: Univariate problems
Previous: NONSTATIONARITY
Stanford Exploration Project
10/21/1998