Basal Banff mixed clastic-carbonate reservoirs are found in the downslope portion of Banff clinoforms. A refined depositional model has been generated based on core and stratigraphic interpretation. Basal Banff reservoirs are characterized using petrophysical analysis, core analysis and facies reconstruction. Exshaw thermal maturity controls the hydrocarbon phase windows. Prospect and regional scale resource-in-place maps are the key output.

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