The spreading surfaces for
the theoretical impulse response of the
common-azimuth migration operator (Appendix F) are
shown in
Figures
and
for the single-mode case, and the converted-mode case,
respectively.
Figure
shows the PP spreading surface in
midpoint-offset coordinates
for an event with a total traveltime of
0.300 s, a P-velocity of 2500 m/s, and inline-offset of 200 m.
Figure
shows the equivalent
PS spreading surface using an S-velocity of 2000 m/s.
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Figures
and
represents the impulse response for
PS common-azimuth migration downward-continuation operator.
Figure
shows the result using the
same velocity for the propagation of the downgoing and upgoing wavefields, which
is equivalent to the single-mode common-azimuth operator.
Figure
shows the result
with a different propagation velocities for each of the two
wavefields, which represents the converted-wave common-azimuth
operator.
Figures
and
are a four-dimensional representation of
the prestack
image with dimensions (
).
For both figures, the top
panel shows the inline-midpoint and crossline-midpoint
cube that corresponds to zero inline subsurface-offset. And,
the bottom panel shows the inline-midpoint and inline subsurface-offset
cube that corresponds to zero crossline-midpoint.
The depth slices in Figures
and
exhibits interesting characteristics of the common-azimuth operator.
For the single-mode case, Figure
, the depth slice
that corresponds to the
inline-midpoint and crossline-midpoint cube (top panel)
shows a circle, whereas the depth slice for inline-midpoint and
inline subsurface-offset
sections (bottom panel) shows a rectangle.
For the converted-mode case, Figure
, the depth slice
in the
inline-midpoint and crossline-midpoint cube
(top panel) has similar characteristic as the single-mode case.
However, the depth slice for the inline-midpoint and inline subsurface-offset
sections (bottom panel)
displays a rectangle
that has been sheared and rotated.
This deformation is the result of using
two different propagation velocities for
the downgoing and upgoing wavefields.
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To validate the implementation of the PS-CAM operator,
I compare the PS impulse response with the
spreading surfaces, which represent the theoretical
solution.
Figure
shows several sections for the
PS impulse response with the
theoretical solution superimposed (blue dotted curve).
This figure shows two panels side-by-side, each panel consists of
five sections. The left panel
shows inline-midpoint sections for zero crossline-midpoint,
and the right panel displays crossline-midpoint sections for zero inline-midpoint.
All the sections correspond to zero subsurface-offset.
Each row represents an impulse response that corresponds to an
spike located at different surface-offset locations.
From top to bottom,
the surface-offsets are:
-250 m, -150 m, 0 m, 150 m, and 250 m, respectively.
Notice that the center panel, that corresponds to zero offset,
the impulse response is completely symmetric, as it is expected.
The asymmetry characteristic for the PS-CAM operator
is observed along the inline direction for different offset values,
as it can be seen along the inline sections (left panel)
in Figure
.
However, the crossline-midpoint location
is symmetric (right panel in Figure
).
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Since the prestack image is four-dimensional, I use another comparison
to truly validate the PS-CAM implementation. The second test corresponds
to an spike located at a fixed surface-offset of 200 m, I take
five inline-midpoint sections that correspond to different
crossline-midpoint locations, and vice versa.
Figure
shows these sections,
the left panel represents the inline-midpoint sections for five
different crossline-midpoint locations. The
right panel displays the crossline-midpoint sections for five
different inline-midpoint locations, all the sections correspond
to zero subsurface-offset.
Both, the inline-midpoint and crossline-midpoint locations
are, from top to bottom,
-250 m, -150 m, 0 m,
150 m, 250 m, respectively. As in the first comparison, the
theoretical solution is superimposed on the PS impulse response
as the blue dotted curve, in this case the spreading surface in
Figure
shows the theoretical solution.
![]() |
.
This figure represents a fixed surface-offset of 200 m,
the left panel represents the inline-midpoint direction and the right panel
the crossline-midpoint direction, all of them corresponds to
zero subsurface-offset. From top to bottom I present
sections at different inline and crossline position: -250 m, -150 m, 0 m,
150 m, 250 m.