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The semi-circle superposition method allows us to visualize how the plume is
built up from constructive interference. It does not, however, offer a
convenient way to numerically compute the actual shape of the plume.
A more effective way to compute the time-migration response to
a point diffractor
is by summing along
hyperbolas Schneider (1978).
The analytical technique for summing along hyperbolas is called the ``common-
tangent'' construction.
It relies on the fact that the main contribution to the sum
comes from the
place where a time-migration hyperbola is tangent to the
true-diffraction curve of
Figure 2. The event at the tangency point is positioned
by time migration to the apex of the time-migration hyperbola.
The time migration hyperbola is given by:
| ![\begin{displaymath}
{t_0^2} = {t_k^2} + 4{[{x_0 - x_k \over V(x_m ,t_m)}]}^2\end{displaymath}](img1.gif) |
(1) |
Matching the slope of the hyperbola given by equation(1)
with the time dip D of the event leads to the following
formulas for the position of the time migrated point (xk,tk):
| ![\begin{displaymath}
x_k = x_0 - {[{V(x_m,t_m)D \over 2}] [{V(x_m,t_m)t_0 \over 2}]}\end{displaymath}](img2.gif) |
(2) |
| ![\begin{displaymath}
t_k = t_0 \sqrt {1 - {[{V(x_m,t_m)D \over 2}]}^2}\end{displaymath}](img3.gif) |
(3) |
where

is the apparent time dip of the event to be migrated and V(xm,tm) is the
RMS well velocity at the diffractor location.
This
procedure is then carried out for each point along the true-diffraction
curve to yield the complete response of time migration to a point
diffractor.
Details of the algebra of
this computation are given in the Appendix and
the results are shown in Figure 5. In generating this
figure we have again used the vertical RMS well velocity that was
used in Figure 3.
Note that
the plume envelope in
Figure 4 matches the curve in Figure 5 exactly.
Thus the two ways of geometrically constructing
the time-migration response to lateral velocity variation are consistent with
each other.
vwell
Figure 5 Plume derived by hyperbola summation with the common-tangent construction.
This curve corresponds to the envelope of semicircles in Figure 4 exactly.
Next: KIRCHHOFF MODELING AND MIGRATION
Up: GEOMETRICAL CONSTRUCTION OF PLUMES
Previous: Semicircle Superposition
Stanford Exploration Project
11/17/1997