Mineralization in the Abloviak study area consists of base metal concentrations within the Tasiuyak Gneiss unit, including Ni + Zn in massive sulfide-graphite horizons (Little Balls, and Cu + W mineralization in calcareous and quartzitic rocks (Pointe Verte; and Cu anomalies in a deformed mafic intrusion (Pointe Verte). Also consists of low base metal concentrations within graphite in post-D2 fault zones (Char Bay); and kimberlite dykes with diamondiferous potential.
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