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Location: 110 km W from High Level, Alberta, Canada
639 – 5th Avenue SW, Suite 1925CalgaryAlberta, CanadaT2P 0M9
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Primary geologic targets of subsurface lithium enriched brines across the Rainbow Lake Lithium Project (RLP) area, are hosted within the Devonian aged Elk Point Group (Sulphur Point, Muskeg and Keg River Formations) of northwestern Alberta. The Elk Point Group aquifers are ideal candidates for sourcing subsurface lithium enriched brines for the purpose of Direct Lithium Extraction (DLE) due to their depositional and reservoir attributes. With a gross thickness exceeding 200 meters (m), and its overall expansive aerial extent, the Elk Point Group represents a known active aquifer system that has produced significant volumes of water associated with historical oil and gas production across the RLP area. Reservoir attributes associated with Elk Point Group primary lithology (e.g.,dolomite) provide significant pore volume and storage capacity of subsurface brines. In addition, high porosity and associated permeability values contribute to the ability of the aquifer to deliver significant production rates over a long period of time.The Middle and Upper Keg River reefs formed on a carbonate platform created by the Lower Keg River Formation. They grew in small basins surrounded by carbonate shelves and the basins were later filled with Muskeg evaporites, which act as a seal for the traps. The Upper Elk Point Group carbonate strata within the Rainbow Lake Property area can be divided into four distinct paleogeographic regions: the Western Platform Edge/Slope (also known as the Comet Platform), Southern Basin, Northern Basin, and Eastern Platform Edge/Slope.
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