Calc-alkaline to tholeiitic and lesser MORB-like basaltic volcanism at 2.66 Ga.
Mesoarchean basement underlying the 2.66 Ga Rankin Inlet greenstone belt.
Intercalated 2.66 Ga and ≤2.50 Ga volcano-sedimentary panels.
Gold linked to 1.9 Ga reworking at cratonic margin and favourable lithostratigraphy.