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Volcanogenic massive sulfide VMS deposits and prospects are hosted in the Middle Devonian to Early Mississippian age Ambler Sequence, a group of metamorphosed bimodal volcanic rocks with interbedded tuffaceous, graphitic and calcareous volcanoclastic metasediments. The Ambler Sequence occurs in the upper part of the Anirak Schist, the thickest member of the Coldfoot subterrane.
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