08/31/2026
The Red Lake greenstone belt contains seven distinct geological assemblages. The Balmer Assemblage, the oldest at 2.98 to 2.96 billion years, hosts every major producing mine in the district, including the former Goldcorp High Grade zone and the Campbell mine. Our Rebel Gold Deposit sits within Balmer Assemblage rocks. The younger Confederation Assemblage, formed roughly 200 million years later, makes up the northern and southern flanks of the belt. These rocks share similar structural controls on gold mineralization but have received significantly less systematic gold-focused exploration. Our Confederation Belt targets sit within this younger package: same district, same structural plumbing, but a largely untested geological frontier.
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