Footwall-type Cu-Ni-PGE mineralization.
Situated in intensely brecciated zones of the footwall (Sudbury Breccia), 1,300 and 500 m, respectively, north of the present Sudbury Igneous Complex-footwall contact.
Mineral List
28 entries listed. 27 valid minerals.
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References
Econ. Geol. 103 (2008) 1005-1028.
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