Please use this identifier to cite or link to this item: https://knowledgecommons.lakeheadu.ca/handle/2453/5339
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dc.contributor.authorKowalski, Barbara Sylvia-
dc.date.accessioned2024-06-20T13:25:57Z-
dc.date.available2024-06-20T13:25:57Z-
dc.date.created1993-
dc.date.issued1993-
dc.identifier.urihttps://knowledgecommons.lakeheadu.ca/handle/2453/5339-
dc.description.abstractThe gold-bearing Metalore shear zone and Golden Highway quartz-carbonate vein in the Beardmore-Geraldton Archean Greenstone Belt occur along the Paint Lake splay faults at the contact between metavolcanic rocks and metaconglomerates intruded by pre-ore diorite. The Metalore and Golden Highway deposits were emplace during a late tectonic event. The consist primarily of quartz, clinochlore, ankerite, potassium feldspars, sericite, pyrite, argentite and chalcopyrite with native gold. The minearls have been deformed and are cut by at least three healed fractures by fluid inclusions. Gold typically occurs in recrystallized quartz. Microthermometric and Raman spectroscopy techniques were used to study fluid inclusions in quartz, calcite, ankerite, chlorites and potassium feldspars. [...]en_US
dc.language.isoen_USen_US
dc.titlePetrographic and fluid inclusion studies on the Metalore-Golden highway deposit, Thunder Bay District, Ontarioen_US
dc.typeThesisen_US
etd.degree.nameMaster of Scienceen_US
etd.degree.levelMasteren_US
etd.degree.disciplineGeologyen_US
etd.degree.grantorLakehead Universityen_US
Appears in Collections:Retrospective theses

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