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APPENDIX A

In Cartesian coordinates, the eikonal equation is

\begin{displaymath}
\tau^2_x(x,z;x_c)+\tau^2_z(x,z;x_c) = s^2(x,z)
\eqno(A.1)\end{displaymath}

where xc=xs or xr are shot or receiver position. Taking partial derivative of both sides of equation (A.1) with respect to xc gives

\begin{displaymath}
2\tau_x(x,z;x_c)\tau_{xx_c}(x,z;x_c)+2\tau_z(x,z;x_c)\tau_{zx_c}(x,z;x_c) = 0.
\eqno(A.2)\end{displaymath}

The right-hand side of the equation is zero because the slowness model is independent of shot-receiver position. Assume the derivatives of the traveltimes are continuous functions of (x,z) and xc, we have

\begin{displaymath}
\begin{array}
{lllll}
p_x(x,z;x_c) & = & \tau_{x_cx}(x,z;x_c...
 ...x_cz}(x,z;x_c) & = & \tau_{zx_c}(x,z;x_c).\end{array}\eqno(A.3)\end{displaymath}

Combining equations (A.2) and (A.3) gives

\begin{displaymath}
\tau_x(x,z;x_c)p_x(x,z;x_c)+\tau_z(x,z;x_c)p_z(x,z;x_c) = 0.
\eqno(A.4)\end{displaymath}

Using the relations between Cartesian coordinates and polar coordinates:

\begin{displaymath}
\left\{
\begin{array}
{lll}
x & = & x_c+r\sin \theta \\ z & = & r\cos \theta,\end{array}\right.
\eqno(A.5)\end{displaymath}

we can derive

\begin{displaymath}
\tau_r(r,\theta ;x_c)p_r(r,\theta;x_c)+{1 \over r^2}\tau_\theta(r,\theta;x_c)p_\theta(r,\theta;x_c) = 0.
\eqno(A.6)\end{displaymath}

 


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Next: About this document ... Up: Zhang: Residual depth migration Previous: References
Stanford Exploration Project
12/18/1997