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 | 阿根廷vs墨西哥竞猜 | en_us |
