A five kilometer long 3C-2D seismic line was acquired by CREWES near Jumpingpound (west of Calgary, Alberta) in 2002. The migrated vertical component stack shows a clear image of the eastern flank of the triangle zone in the study area. The radial component shot gathers are quite noisy, but coherent reflections can be identified on the migrated stack. The vertical and radial component stacks compare well, and it should be possible to conduct a joint interpretation study.
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