next up previous print clean
Next: A real dataset: ExxonMobil Up: Numerical examples Previous: Impulse response

A synthetic dataset

Figures [*]-[*] show a synthetic model for VTI media. Figure [*] is the velocity model, Figure [*] is the map of the anisotropy parameter $\varepsilon$, and Figure [*] is the map of the anisotropy parameter $\delta$. There are 720 shots in total and the maximum offset for each shot is 8000 meters. The challenging part of this model is to accurately image the steep fault, salt flank and the two abnormal sediments near the right corner of the salt body. I run a plane-wave migration, using the optimized implicit finite-difference operator as the extrapolator. I generate 70 plane-wave sources, for which the take-off angles at the surface range from $-40^\circ$ to $40^\circ$. Figure [*] shows the image. Notice that the steeply dipping salt flank and the fault are well imaged. The steepest part of the salt flank is about $60^\circ$.The abnormal sediments also are well imaged.

 
vpani
vpani
Figure 4
Vertical velocity model.
view burn build edit restore

 
epsani
epsani
Figure 5
Anisotropy parameter $\varepsilon$.
view burn build edit restore

 
dltani
dltani
Figure 6
Anisotropy parameter $\delta$.
view burn build edit restore

 
imfdhess
imfdhess
Figure 7
Implicit finite-difference migration.
view burn build edit restore


next up previous print clean
Next: A real dataset: ExxonMobil Up: Numerical examples Previous: Impulse response
Stanford Exploration Project
4/5/2006