The phase-shift method of migration is attractive because
it allows for arbitrary depth variation in velocity and
arbitrary angles of propagation up to 90.Unfortunately, lateral variation in velocity is not permitted
because of the Fourier transformation over the x-axis.
To alleviate this difficulty, Gazdag and Sguazzero [1984]
proposed an interpolation method.
Recall from chapter
that the phase-shift method
2-D Fourier transforms the data p(x,t) to
.Then
is downward continued
in steps of depth by multiplication
with
.Gazdag proposed several reference velocities, say, v1,
v2,
v3,
and
v4.
He downward continued one depth step with each of the velocities,
obtaining several reference copies of the downward-continued data, say,
P1,
P2,
P3,
and
P4.
Then he inverse Fourier transformed
each of the Pj
over kx to
.At each x, he interpolated the reference waves of nearest velocity
to get a final value, say,
which
he retransformed to
ready for another step.
This appears to be an inefficient method since it duplicates the usual
migration computation for each velocity.
Surprisingly, the method seems to be successful,
perhaps because of the peculiar nature
of computation using an array processor.