Please use this identifier to cite or link to this item: https://zone.biblio.laurentian.ca/handle/10219/3693
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dc.contributor.authorRush, Louise Victoria-
dc.date.accessioned2021-06-08T18:21:40Z-
dc.date.available2021-06-08T18:21:40Z-
dc.date.issued2021-04-29-
dc.identifier.urihttps://zone.biblio.laurentian.ca/handle/10219/3693-
dc.description.abstractThe recent emergence of Co as a critical metal used in a variety of high-technology industries has refocused exploration at Cobalt, Ontario. This district represents an unusual ore deposit-type termed the five-element (Ag-Ni-Co-As-Bi) assemblage and was important historically as Canada’s former premier Ag producer at over 460 Moz (1904-1989). This study applies a sophisticated analytical protocol consisting of whole rock analysis, petrography, and insitu mineral analyses (SEM-EDS, LA-ICP-MS) to a sample suite with spatial coverage across the district. These methods constrain geological controls on regional metal distribution, the sequence of alteration and mineralization, and the physiochemical evolution of the system. An updated genetic model for the mineralization involves the veins representing a district-scale homogeneous hydrothermal-metal melt system driven by contact metamorphism and partial melting of pre-existing sulfides in underlying Archean basement rocks. This model enhances understanding of deposit formation and offers refined geochemical vectors to aid ongoing exploration efforts.en_US
dc.language.isoenen_US
dc.subjectCobalten_US
dc.subjectfive-element mineralizationen_US
dc.subjectarsenidesen_US
dc.subjectreductionen_US
dc.subjectmetal melten_US
dc.subjectmetal zonationen_US
dc.subjectcoupled dissolution-precipitationen_US
dc.titleA new model for an old camp: the enigmatic Ag-Co-Ni-As-Bi mineralization of Cobalt, Ontarioen_US
dc.typeThesisen_US
dc.description.degreeMaster of Science (MSc) in Geologyen_US
dc.publisher.grantorLaurentian University of Sudburyen_US
Appears in Collections:Geology - Master's Theses

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