
The Gorman Project covers a ~45km long segment of the Favourable Lake greenstone belt, which forms part of the Sachigo Terrane, Archean Superior Craton. The terrane is bound by the Bearhead Lake fault zone, a regional-scale structure that is interpreted as a first-order control on the emplacement of LCT pegmatites and their parental granitic intrusions.
The Project captures several mapped pegmatitic granite occurrences, including a potentially fertile, peraluminous, coarse grained to pegmatitic two-mica granite, which is similar in nature to and along strike from the Pakeagama Lake granite that hosts Frontier Lithium’s PAK deposit. Fertile granites are interpreted to be the parental rocks that give rise to LCT pegmatites.


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