GEOTHERMAL RESOURCE CHARACTERIZATION OF THE SLAVE POINT FORMATION IN CLARKE LAKE FIELD, FORT NELSON, B.C., CANADA
We describe and map depositional facies and relate these to porosity and permeability data to determine a flow model for the formation. In the late Givetian a relative sea level rise drowned the Keg River carbonate platform which allowed small, laterally discontinuous patch reefs of the Slave Point Formation to develop on the flanks of the Horn River Basin. Nine depositional facies have been described by Lonnee (2005) of which eight are coincident with Machel & Hunter’s (1994) reef facies classification. Pervasive dolomitization of the reef margin occurred by long-distance migration of halite-saturated brines while recrystallized matrix dolomite, replacive and cement saddle dolomites are products of hydrothermal alteration. More porous and permeable zones are related to dolomitization, while unaltered limestone facies are considered non-reservoir. Mapping and modeling the spatial variability of dolomitization is a key objective concerning optimization of geothermal well targets.
The feasibility of developing this geologically based geothermal reservoir model comes in part to the availability of a large-scale oil and gas well data set. The data include direct permeability/porosity core measurements, well-logs, DSTs and twenty core descriptions taken at the BC Oil & Gas Commission core research facility. Over 220 wells in the Clarke Lake area have been used in conjunction with the software Petrel to create stratigraphic cross-sections to interpret the 3D geometry of the reef.