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PGE–Cu–Ni sulfide mineralization of the mesoproterozoic Escape intrusion, northwestern Ontario
(2023)
The Escape intrusion is a tabular to bladed, mafic–ultramafic chonolith that hosts
economic concentrations of PGE–Cu–Ni magmatic sulfide mineralization. The Mesoproterozoic
intrusion is located about 50 km northeast of ...