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Age and geological setting of the Rankin Inlet greenstone belt and its relationship to the gold endowment of the Meliadine gold district, Nunavut, Canada
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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.

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