It consists of mafic-ultramafic rocks and is the largest of many mafic-ultramafic intrusions associated with felsic and mafic metavolcanic rocks in the northern Archean Temagami Greenstone Belt.
[1] Five magmatic cycles have been identified in the Kanichee layered intrusive complex, the first of which formed a PGE deposit with associated gold, copper and nickel mineralization.
Ore mineralogy includes pyrrhotite, pentlandite, chalcopyrite and pyrite.
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