DOI: 10.22215/etd/1986-01157
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Geological setting, structure, and alteration associated with gold-pyrite mineralization in mafic volcanic rocks at Cameron Lake, Wabigoon subprovince, northwestern Ontario.

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“…However, over 60% of the gold endowment originates from quartz-carbonate veins formed during late-stage tectonic inversion of the extensional basins [49]. In the Wabigoon subprovince, many gold deposits and prospects are interpreted as orogenic gold, including the areas of mineralization within the Cameron Lake area hosted by the Cameron-Pipestone deformation zone [50,51]. This type of gold mineralization is the focus of the present study.…”
Section: Introductionmentioning
confidence: 91%
“…However, over 60% of the gold endowment originates from quartz-carbonate veins formed during late-stage tectonic inversion of the extensional basins [49]. In the Wabigoon subprovince, many gold deposits and prospects are interpreted as orogenic gold, including the areas of mineralization within the Cameron Lake area hosted by the Cameron-Pipestone deformation zone [50,51]. This type of gold mineralization is the focus of the present study.…”
Section: Introductionmentioning
confidence: 91%