Image Gallery

ALL ALBUMS » Gallery » 32867
Figure 4: (a) Time slices at t=1300 ms through fault probability volumes computed with two passes of Kuwahara principal component structure-oriented filtering. Discontinuities subparallel to reflector dip have been suppressed. Note the improved continuity and extent of the faults where the fault enhancement algorithm has joined previously disjoint fault segments. (b) The seismic volume co-rendered with the fault probability volume, providing a useful way of carrying out fault interpretation.
(6 of 6)
Figure 4: (a) Time slices at t=1300 ms through fault probability volumes computed with two passes of Kuwahara principal component structure-oriented filtering. Discontinuities subparallel to reflector dip have been suppressed. Note the improved continuity and extent of the faults where the fault enhancement algorithm has joined previously disjoint fault segments. (b) The seismic volume co-rendered with the fault probability volume, providing a useful way of carrying out fault interpretation.