The Abitibi Sub-province extends from Timmins, ON to Val d’Or, QC and contains gold deposits with equivocal genesis, derived from either magmatic or metamorphic processes. The largest of the gold lode deposits precipitated at paleotemperatures and paleopressures indicative of depths 8-12 km below the surface. Metal-rich fluid flow at these depths through structurally deformed rocks […]
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