I display the source function on the left panel,
and the recorded wavefield on the right panel. The
recorded wavefield is the superposition of primaries and multiples.
The migration result for this shot location is shown in Figure
a.
Figure
displays the source function and the
up-going wavefield for the migration of multiples. As proposed in the
preceding section, the source function is not impulsive but areal.
The recorded wavefield contains the surface-related multiples only.
The migration result is shown in Figure
b and
compares favorably with the output of the migration of primaries.
It is interesting to note that the water-bottom is illuminated with
a wider aperture when multiples are used. As illustrated in Figure
, for a given receiver Rn, the primary illuminates
the reflector in ra at a closer location to the source in S
than does the multiple in rb. Therefore, for one given shot, the
multiples migrate with a wider aperture but with smaller angles.
As a final result, I display in Figures
c and
d
the different illumination patterns for both the impulsive and areal
sources ().
These maps are obtained by simply computing the amplitude
(squared) of the down-going wavefield at each depth and for each
frequency. These Figures illustrate the aperture and illumination
effects of the multiples.
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