Region Growing produced a very different image of the K-8/16 reservoirs. The tubular nature and inter-twining of turbidite fairways can be seen. The K-8 reservoir is a gas depletion drive, and indeed, brightening over time is observed throughout most of the reservoir. Two wells weire produng in the study area between 1088 and 1994, and in both, gas production increased dramatically over time.
Although we were not able to differentiate between K-8 and K-16 sands using region growing, the 4D analysis may have identified certain tunes in the south as K-16, since there dimming of amplitudes was observed, andthe K-16 is a water drive reservoir. The 3D brihtening and dimming of th esean package may be able to discern which is K-8 vs K-16 farther north.
