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Imaging principle

One of the advantages of the choice of the midpoint-offset coordinate to migrate the data is that the imaging step is both straightforward and inexpensive. There is no need to crosscorrelate and shift wavefields, as for shot-profile reverse-time migration Biondi (2002).

The equivalent of the ``stacked'' image is obtained by selecting the propagated wavefield at zero time and zero offset; that is  
 \begin{displaymath}
I\left(z, x_m\right) =
P\left(t=0,z,x_m,x_h=0 \right)\end{displaymath} (12)
The offset-domain Common Image Gathers (CIG) are obtained by simply selecting the propagated wavefield at zero time; that is  
 \begin{displaymath}
I\left(z, x_m, x_h\right) =
P\left(t=0,z,x_m,x_h\right).\end{displaymath} (13)


next up previous print clean
Next: Examples of reverse time Up: From downward continuation to Previous: Stronger lateral velocity variations?
Stanford Exploration Project
6/7/2002