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Conclusions

This work has presented a 2-D and 3-D extended split-step migration algorithm that uses the evanescent energy to image steep events in strong lateral gradients. Our results show that evanescent energy helps to image steep events in a strong lateral velocity gradients. In addition, the imaging of steep events depends on the number of reference velocities in order to accommodate the lateral velocity gradient, thus increasing the number of calculations.


next up previous print clean
Next: Acknowledgments Up: Rickett, et al.: STANFORD Previous: Results
Stanford Exploration Project
7/5/1998