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  • Gathering Lake and Triangle Lake: 8,938 hectares collectively within the prolific Georgia Lake pegmatite field, east of Rock Tech Lithium’s Georgia Lake Deposit, which hosts a 10.6 Mt indicated resource at 0.88% Li2O and 4.22 Mt inferred resource at 1.04% Li2O, and Imagine Lithium’s Jackpot Discovery which has identified 25.5 metres at 1.21% Li2 Lithium occurrences in this field run along a primary fault which runs through Triangle Lake and is adjacent to Gathering Lake, suggesting that the mapped pegmatites on these properties may be highly fractionated LCT-pegmatites that bear spodumene.


To Be Announced

* Generalized exploration model for LCT pegmatites. Pegmatites exhibit a high degree of zonation, whereby different portions of the pegmatite body may contain different minerals. Mineralization is spatially related to the source; barren pegmatites are more likely to occur at the granitic source, but as one moves more distal, the pegmatites are expected to increase in tantalum, then lithium, and then cesium. The presence of beryl, tantalum, and cesium indicates that the White Willow pegmatites are highly fractionated and very prospective for the presence of lithium as this zone is the “outer zone” that is most distal from the granitic source. Source: USGS (modified from Trueman and Cerny, 1982).

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