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From Figure we can immediately compute the takeoff
angle of the diffracted receiver ray as
| |
(78) |
mul_sktch13
Figure 26 Sketch showing the
geometry of the zero surface half-offset diffracted multiple from a
dipping water-bottom.
|
| |
In this equation the depth of the diffractor is not known, but it can be
calculated from the geometry of Figure :
| |
(79) |
As we did for the diffracted multiple from the flat water-bottom, we can
use the traveltime of the multiple at the zero surface-offset trace to compute
, except that this time the computation is much more involved.
Figure shows the basic geometry. From triangle ABC we
have
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(80) |
were tr1 is the traveltime of the diffracted segment that, according
to triangle DEF in Figure is given by
|
[V1tr1(0)]2=Zdiff2+(Xdiff-mD)2.
|
(81) |
Replacing equations 79 and 81 into equation 80
gives a quartic equation for which can be solved numerically.
Once is known, we can easily compute Zdiff with
equation 79 and therefore with equation 78
in terms of the known quantities hD, mD, Xdiff and tm(0).
mul_sktch15
Figure 28 Sketch to compute
the takeoff angle of the source ray from a diffracted multiple.
|
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In order to compute , we apply the law of sines to triangle ABC
in Figure to get
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(82) |
where and V1tr1 is the
length of the diffracted receiver ray and is given by
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(83) |
Therefore, plugging equation 83 into equation 82 we get
equation 50:
| |
(84) |
Next: About this document ...
Up: Alvarez: Multiples in image
Previous: From dip to no
Stanford Exploration Project
11/1/2005