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Next: 11: TRUE AMPLITUDE MIGRATION Up: Goldin: Method of discontinuities Previous: Very simple but important

10: EXTREMAL VELOCITIES

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 $w({\bf r},r)$, 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} (102)
and  
 \begin{displaymath}
{\partial ^2 T(x,z,r) \over {\partial r^2}} - {{d^2 \tau_0}\over {dr^2}} = 0.\end{displaymath} (103)

If at some velocity vc = vex the caustic and the image cross each other at a special point ${\bf r}$, we call this the extremal velocity vex. Usually we have a continuous interval of extremal velocities: $v_{ex} \in V_{ex}$.Typically for each $v_{ex} \in V_{ex}$ 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):
\begin{eqnarraystar}
\xi (\theta)& =& [1-{{({v_c \over v})^2 - \sin^2\theta } \o...
 ...ver {\cos^3 \theta}} \sqrt{1 - ({v_c \over v})^2 \sin^2\theta}\end{eqnarraystar}

To find the location of caustics, we substitute $\tau_0(r) = {1 \over v} \sqrt{r^2 + 4 h^2}$ and $T(x,z,r)={1 \over v_c} 
\sqrt{(r-x)^2 + z^2}$.into system equations (102) and (103). So we have the system of equations
\begin{eqnarraystar}
{r \over {v \sqrt{r^2+4 h^2}}} = { {r-x} \over {v_c \sqrt{(...
 ...= {1 \over v_c} { {z^2} \over {((r-x)^2 + z^2)^{3 \over 2}} }.\end{eqnarraystar}

If for some $\theta$ and r we have $\xi = x$ and $\eta = z$, then the reflector's image contains the special point $(\xi ,\eta)$.Calculations show that at vc < v there is no special point on the image. At $v < v_c < \sqrt{2}$ we have two symmetrical special points which merge together into the one bright point when $v_c = \sqrt{2} v \equiv v_{ex}^*$ (as shown in Figure [*]).

Instead of a complete investigation of the situation, we can choose some particular ray of the eikonal $\tau^{(-)}$.It is not difficult to determine the meaning of ${\partial ^2T({\bf r},r)} \over {\partial r^2}$ for the given velocity v=vc and the point ${\bf r}^{\prime}$ belonging to the image and the ray $\gamma$; 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 $\gamma_s$ which approaches the surface $\Sigma$ vertically. This ray is connected with a stationary point rs of the function $\tau_0(r)$:

\begin{displaymath}
{d\tau_0 \over {dr}}\vert _{r=r_s} = 0\end{displaymath}

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 $\tau_0(r_s)=t_s$, then hm satisfies  
 \begin{displaymath}
{h_m \over v_c} + {\sqrt{h_m^2 + r_s^2} \over v_c} = t_s .\end{displaymath} (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} (105)

The point ${\bf r}^{\prime} = (r_s,h_m)$ 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} (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} (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} (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} (109)

As for ${d^2 \tau_0} \over {dr^2}$ 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} (110)
where k is the reflector curvature at point ${\bf r}$. 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} (111)
If the reflector is planar (k=0), then  
 \begin{displaymath}
v_{ex} = v {\sqrt{1+\cos^2 \phi} \over {\cos \phi}}\end{displaymath} (112)

If the point ${\bf r}^{\prime}$ is stationary for the reflector ($\phi = 0$), then  
 \begin{displaymath}
v_{ex} = \sqrt{2} v {\sqrt{{1 + k h} \over { 1+ 2k h}}}\end{displaymath} (113)

If the reflector is planar and horizontal (k=0 and $\phi = 0$), then  
 \begin{displaymath}
v_{ex} = \sqrt{2} v\end{displaymath} (114)
and, at last, if we have a point reflector ($k=\infty$), then

 
vex = v (115)

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}

and at $\phi = 0$

\begin{displaymath}
v_{ex} = v \sqrt{1 + {1 \over {kh}}}\end{displaymath}

If k=0 (planar reflector) we formally receive $v_{ex}=\infty$, 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.


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Next: 11: TRUE AMPLITUDE MIGRATION Up: Goldin: Method of discontinuities Previous: Very simple but important
Stanford Exploration Project
1/13/1998