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Next: Common-azimuth Stolt residual migration Up: Prestack residual migration Previous: Stolt migration

Prestack Stolt residual migration

In general, residual migration improves the quality of an image without re-migration of the original data; instead, a transformation is applied to the current migrated image.

In prestack Stolt residual migration, we attempt to correct the effects of migrating with an inaccurate reference velocity by applying a transformation to images transformed to the Fourier domain. Supposing that the initial migration was done with the velocity v0, and that the correct velocity is v, we can use dsr-sg to derive ${\kzz}_0$, the vertical wavenumber for the reference velocity, and $\kzz$, the vertical wavenumber for the correct velocity.

Mathematically, the goal of prestack Stolt residual migration is to obtain $\kzz$ from ${\kzz}_0$. If we elliminate $\omega$ from ${\kzz}_0$ and $\kzz$,and make the notation $\rho=\frac{v_0}{v}$,we obtain the residual migration equation for full 3D prestack seismic images:  
 \begin{displaymath}
\bea{r}
\kzz= \frac{1}{2}
\sqrt{ \rho^2
\frac{ \lb 4{\kzz}_0...
 ...f k}_s\vert\rp^2\rb}{16{\kzz}_0^2}-\vert{\bf k}_s\vert^2},
\eea\end{displaymath} (33)
which can also be represented in midpoint-offset coordinates using the change of variables in changevar. If we make the change of variables
\begin{displaymath}
\mu^2 = \frac{ \lb 4 {{\kzz}_0}^2 + \lp {\bf k}_r- {\bf k}_s...
 ...}_0}^2 + \lp {\bf k}_r+ {\bf k}_s\rp^2 \rb }
 {16{{\kzz}_0}^2}.\end{displaymath} (34)
we obtain a simplified version of myresmig-3d-pr:
\begin{displaymath}
\kzz = \frac{1}{2}\sqrt{ \rho^2 \mu^2 - \vert{\bf k}_s\vert^2}
 + \frac{1}{2}\sqrt{ \rho^2 \mu^2 - \vert{\bf k}_r\vert^2} \;.\end{displaymath} (35)

In the 3D post-stack case, when ${\bf k}_h={\bf 0}$, myresmig-3d-pr becomes:  
 \begin{displaymath}
\kzz= \sqrt{ \rho^2 \lb {\kzz}_0^2+ \vert{\bf k}_m\vert^2 \rb -\vert{\bf k}_m\vert^2}.\end{displaymath} (36)

In the 2D prestack case (kmy=0 and kmx=0), we can write myresmig-3d-pr as:  
 \begin{displaymath}
\bea{r}
\kzz=\frac{1}{2}
\sqrt{ \rho^2
\frac{ \lb {\kzz}_0^2...
 ...zz}_0^2+{k_m}_x^2 \rb} 
{{\kzz}_0^2}-({k_m}_x-{k_h}_x)^2}.
\eea\end{displaymath} (37)

For 2D post-stack data, myresmig-3d-po and myresmig-2d-pr become  
 \begin{displaymath}
\kzz= \sqrt{ \rho^2\lb {\kzz}_0^2+{k_m}_x^2\rb-{k_m}_x^2},\end{displaymath} (38)
which can also be written in the familiar form (102):  
 \begin{displaymath}
\omega = \sqrt{\omega_0^2+{k_m}_x^2 \lp v_0^2-v^2\rp},\end{displaymath} (39)
where, by definition, $\ww_0= {\kzz}_0 v_0$, and $\ww = \kzz v$.


next up previous print clean
Next: Common-azimuth Stolt residual migration Up: Prestack residual migration Previous: Stolt migration
Stanford Exploration Project
11/4/2004