ABSTRACT
Prestack partial migration (PSPM)
is a well-known process which
transforms the prestack data to zero offset.
I discuss several properties of the PSPM spreading operator
and of the equivalent PSPM summation operator
reflected by a transformation of coordinates from (x, t) domain
to (p, ) domain, where p=2dt/dx and is the NMO
correction. This transformation allows for a more general
representation for the PSPM operator and can explain the
apparition of triplications in the DMO curve in a
variable velocity medium.
Then I attempt to find a partial differential equation formulation
for the PSPM operator in the family of first order partial
differential equations using as characteristics the curves
defined by the new transformation of coordinates.
|