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As the variable
is replaced with
in the integral
![\begin{displaymath}
\int d\omega p(\omega,k_y,k_h)=
\int d\omega_0 {\left[{{d \omega} \over {d \omega_0}}\right]}
p^*(\omega_0,k_y,k_h),\end{displaymath}](img25.gif)
each value of
in the integral
needs to be associated with the appropriate value of the field
which is
.The new field
represents
a remapping of the original field
.Each value in the new field
with
coordinates
corresponds to the value
in the field
with coordinates
.
The
remapping can be understood easier
if one takes the particular case ky=0.
The change of variable in
(5) becomes

the Jacobian
![\begin{displaymath}
{\left[ {{d \omega} \over {d \omega_0}} \right]}=
{{\mid {{2...
...over v} \mid} \over
{\sqrt{{{4\omega_0^2} \over v^2}+k_h^2}}},\end{displaymath}](img33.gif)
and the zero-offset migrated field becomes
|  |
(10) |
Compare equation (10) with the Gazdag (1978) and
Stolt (1978) zero-offset migration equations:
|  |
(11) |
Notice that the Stolt migration formula is comprised of an
inverse Fourier transform and a remapping (interpolation).
Equation (10) inside the integral in kh
has the same form
as the remapping in the Stolt formula, save for a constant
coefficient
. This similitude suggests the equivalent
formulation:
|  |
(12) |
The validity of the new equation is verified
by replacing in equation (12) the
exponential expression

by a new variable
to get back the inverse Fourier transform
of the initial expression.
The integration in kh represents the inverse Fourier
transform at zero offset (h=0). However because
equation (12) actually performs summation along
hyperbolas in the spatial coordinate h, replacing
the integral in kh by the inverse Fourier transform will not
return the constant-offset sections.
Applying the same technique to the case
I obtain
| ![\begin{displaymath}
p_0(t_0,k_y)=
\int dk_h \int d\omega \;
e^{-isign(\omega)
{\...
...h^2)^2-4\omega^2v_y^2})\right]}^{1\over2}t_0}
p(\omega,k_y,k_h)\end{displaymath}](img40.gif) |
(13) |
which can be verified by substituting the exponential
expression in
with a new variable
defined as
| ![\begin{displaymath}
\omega_0^2 = {1 \over 2}
\left [ {\omega^2+v_y^2-v_h^2 +
{\sqrt {(\omega^2+v_y^2-v_h^2)^2-4 \omega^2 v_y^2}}} \right ].\end{displaymath}](img42.gif) |
(14) |
Next: PDE
Up: Introduction
Previous: MZO from prestack migration
Stanford Exploration Project
11/17/1997