Using 3-D Seismic Coherency and Stratal Surfaces to Optimize Redevelopment of Waterflooded Reservoirs, Cut Bank Field, Montana |
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Contents
Abstract | 1 |
Time slice across amplitude volume at 432 ms | 8 |
Time slice across coherence volume at 600 ms | 14 |
1 other sections not shown
Common terms and phrases
1.0 km Figure 200 Crossline coordinate 3-D seismic data 3-D seismic survey 3-D seismic volume 3-D survey active injector adjacent traces amplitude volume Average absolute amplitude Bank sand unit bentonite layer bounding stratal surfaces Channel system Clay plugging coherence volume cross-correlation Crossline coordinate 250 Cut Bank field Cut Bank Member Cut Bank sand define depositional environments East Inline coordinate Economic Geology Edge of incised Ellis Group frequency bandwidth Geology Glacier County gross sand thickness Hardage hydrocarbon incised valley 100 incised-valley systems Inline coordinate 300 lower bounding stratal lower Cut Bank Montana MSR Exploration receiver lines reflection amplitudes reflection waveshapes reservoir compartmentalization reservoir sands SCCBSU seismic reflection character slice across amplitude slice across coherence STRATAL SURFACE IMAGING stratigraphic study area Sweetgrass thin beds thin-bed tion Type-log unconformably upper Cut Bank UPPER JURASSIC vertical seismic profile Vertical seismic section volume at 432 VSP data VSP image VSP reflection character West edge