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Prestack depth migration of reflectors is a two-step
process: focusing followed by mapping.
In conventional processing the focusing is accomplished by
normal moveout (NMO) followed by stacking, while
the mapping is provided by poststack depth migration.
In presence of dipping reflectors the NMO step must be
followed by dip-moveout to properly focus the
reflections from dipping beds.
Migrating the data in two steps has some advantages with
respect to migrating it in only one step.
One theoretical advantage is that focusing produces
a result in time and not in depth, therefore focusing
enhances the reflectors in a zero offset
section but does not affect their position.
This property of focusing satisfies both
the conservatives, who think that velocity cannot be
estimated well enough to rely on the result of
mapping, and the anisotropic people,
who believe that horizontal (focusing) velocities and
vertical (mapping) velocities are different.
Efficiency is the other important advantage in splitting
the migration process.
Only the stacked data is mapped to depth and the
whole prestack data is focused instead of
being fully migrated.
Next: DMO
Up: Popovici and Biondi: PSPM
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Stanford Exploration Project
1/13/1998