Seafloor deposit models, geochemistry, and petrology of the mafic-ultramafic hosted Big Lake VMS occurrence, Marathon, Ontario
| dc.contributor.advisor | Hollings, Peter | |
| dc.contributor.author | Rinne, Marc L. | |
| dc.date.accessioned | 2012-11-11T02:41:32Z | |
| dc.date.available | 2012-11-11T02:41:32Z | |
| dc.date.created | 2010-05 | |
| dc.date.issued | 2010 | |
| dc.identifier.uri | http://knowledgecommons.lakeheadu.ca/handle/2453/256 | |
| dc.description.abstract | The Big Lake volcanogenic massive sulphide (VMS) occurrence, located in the Schreiber-Hemlo belt of the Superior Province, was discovered in March 2006 near Marathon, Ontario. It is hosted in a mafic-ultramafic metavolcanic sequence lacking felsic volcanic or volcaniclastic rock, and consists of a thin, locally anastomosing sheet of veined pyrrhotite, chalcopyrite, and sphalerite currently defined over a plan area of approximately 0.5x0.5 km, along the base of a series of peridotite and pyroxenite cumulates termed the Big Lake Ultramafic Complex (BLUC). | en_US |
| dc.language.iso | en_US | en_US |
| dc.subject | Geochemistry | en_US |
| dc.subject | Ontario, Northwestern | en_US |
| dc.subject | Marathon region | en_US |
| dc.subject | Petrology | en_US |
| dc.subject | Mineralogy | en_US |
| dc.subject | Geology | en_US |
| dc.title | Seafloor deposit models, geochemistry, and petrology of the mafic-ultramafic hosted Big Lake VMS occurrence, Marathon, Ontario | en_US |
| dc.type | Thesis | en_US |
| etd.degree.name | Master of Science | |
| etd.degree.level | Master | en_US |
| etd.degree.discipline | Geology | en_US |
| etd.degree.grantor | Lakehead University | en_US |
