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We know how to determine the image of a reflector's location on a migrated
section. This location, of course, depends on the choice of the continuation
velocity vc. Being independent of a weight function
,
the location of caustics in the
x,z-plane is determined by the system of equations
| ![\begin{displaymath}
{\partial T(x,z,r) \over {\partial r}} - {{d \tau_0}\over {dr}} = 0\end{displaymath}](img597.gif) |
(102) |
and
| ![\begin{displaymath}
{\partial ^2 T(x,z,r) \over {\partial r^2}} - {{d^2 \tau_0}\over {dr^2}} = 0.\end{displaymath}](img598.gif) |
(103) |
If at some velocity vc = vex the caustic and the image cross each other
at a special point
, we call this the extremal velocity vex. Usually
we have a continuous interval of extremal velocities:
.Typically for each
one can observe two or more
special points. For some value vex = v*ex called the true extremal
velocity, these special points unify in one point that appears as a
bright spot.
Example: If the true model represents a homogeneous medium with velocity v
and a planar reflector at depth h, the location of the reflector's image
after CSP-migration is described by the system of equations (see Chapter 7):
To find the location of caustics, we substitute
and
.into system equations (102) and (103).
So we have the system of equations
If for some
and r we have
and
, then the reflector's image contains the special point
.Calculations show that at vc < v there is no special point on the image.
At
we have two symmetrical special points which merge
together into the one bright point when
(as shown
in Figure
).
Instead of a complete investigation of the situation, we can choose some particular ray of the eikonal
.It is not difficult to determine the meaning of
for the given velocity v=vc and the point
belonging to the image and the ray
; we can easily check condition (103).
Let us again consider CSP-migration with the true model containing a curved
reflector in a homogeneous medium (Figure
, solid line). Let us
choose the ray
which approaches the surface
vertically.
This ray is connected with a stationary point rs of the function
:
![\begin{displaymath}
{d\tau_0 \over {dr}}\vert _{r=r_s} = 0\end{displaymath}](img613.gif)
and we shall call this ray stationary. We shall denote h the true depth of the reflector and hm the image depth for the x=rs. If
, then
hm satisfies
| ![\begin{displaymath}
{h_m \over v_c} + {\sqrt{h_m^2 + r_s^2} \over v_c} = t_s .\end{displaymath}](img615.gif) |
(104) |
It is easy to show that
| ![\begin{displaymath}
\left.{{\partial ^2 T} \over {\partial r^2}} \right\vert _{r=r_s,{\bf r}={\bf r}^{\prime}} = {1 \over {v_c h_m}}\end{displaymath}](img616.gif) |
(105) |
The point
belongs to a caustic if
| ![\begin{displaymath}
{1 \over {v_c h_m}} = {{d^2 \tau_0} \over {dr^2}} \vert _{r=r_s}\end{displaymath}](img618.gif) |
(106) |
Using equation (104), we have
| ![\begin{displaymath}
h_m = {{t_s^2 v_c^2 - r_s^2} \over {2 t_s v_c}}.\end{displaymath}](img619.gif) |
(107) |
Combining (106) and (107) we receive
| ![\begin{displaymath}
v_c = v_{ex} = \sqrt{ {2 \over {t_s {{d^2 \tau_0} \over {dr^2}}} } + ({r_s \over t_s})^2}\end{displaymath}](img620.gif) |
(108) |
It is easy to derive (see Figure
)
| ![\begin{displaymath}
r_s = h \tan(2 \phi) , \qquad t_s = {{2 \cos^2 \phi} \over {\cos(2 \phi)}}{h_m \over v_c} .\end{displaymath}](img621.gif) |
(109) |
As for
we can use standard techniques based on the continuation of wave front curvatures along the ray. We shall omit all these calculations and give the final result:
| ![\begin{displaymath}
{{d^2 \tau_0} \over {dr^2}} \vert _{r=r'} = {1 \over {v h}} ...
...cos \phi~\cos(2 \phi) + 2 k h} \over { 2 ( \cos^3 \phi + k h)}}\end{displaymath}](img623.gif) |
(110) |
where k is the reflector curvature at point
. Substitution of equations
(109) and (110) into (108) gives
| ![\begin{displaymath}
v_{ex} = {{\sqrt{2} v} \over {\cos \phi}} \sqrt{ {{\cos (2 \...
... {\cos \phi~\cos (2 \phi) + 2 k h}} + {1 \over 2} \sin^2 \phi }\end{displaymath}](img624.gif) |
(111) |
If the reflector is planar (k=0), then
| ![\begin{displaymath}
v_{ex} = v {\sqrt{1+\cos^2 \phi} \over {\cos \phi}}\end{displaymath}](img625.gif) |
(112) |
If the point
is stationary for the reflector (
), then
| ![\begin{displaymath}
v_{ex} = \sqrt{2} v {\sqrt{{1 + k h} \over { 1+ 2k h}}}\end{displaymath}](img627.gif) |
(113) |
If the reflector is planar and horizontal (k=0 and
), then
| ![\begin{displaymath}
v_{ex} = \sqrt{2} v\end{displaymath}](img628.gif) |
(114) |
and, at last, if we have a point reflector (
), then
Is this velocity vex the true extremal velocity?
It is in all particular situations expressed by formulas (112) -
(115).
In the zero offset case for arbitrary rays
![\begin{displaymath}
v_{ex} = v \sqrt{ {1 + k h \cos \phi} \over {1 + k h \cos \phi~\sin^2 \phi}}\end{displaymath}](img630.gif)
and at
![\begin{displaymath}
v_{ex} = v \sqrt{1 + {1 \over {kh}}}\end{displaymath}](img631.gif)
If k=0 (planar reflector) we formally receive
, but in this case
the amplitude does not actually depend on the meaning of the velocity vc.
In the common mid-point case travel-time curves for a point reflector and for
a flat reflector are the same. It means that in this situation vex=v.
Next: 11: TRUE AMPLITUDE MIGRATION
Up: Goldin: Method of discontinuities
Previous: Very simple but important
Stanford Exploration Project
1/13/1998