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Next: Simple Amplitude Boundary Up: Lomask and Biondi: Image Previous: Application to seismic

Test Cases

We applied this segmentation technique to two simple models of salt boundaries and a 2D field seismic section. The first model tests a simple continuous salt boundary. The second model introduces a discontinuity into the salt boundary that would cause conventional auto-trackers to fail. Finally, the 2D seismic section tests this method on real data with a salt boundary that would be difficult for conventional trackers to follow.