Figure 10. Ant Cube viewed as time slice to guide fault interpretation, while the vertical section is the structural smoothed seismic interpretation of horizons. Horizon can be auto-picked initially from smoothed seismic for regional extend, then snapped to original seismic for amplitude extraction. The faults can be auto-picked from the edge volume, manually interpreted (red) on the time slices, or automatically extracted from the data as surfaces (Figure 9).