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http://hdl.handle.net/11375/17818
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DC Field | Value | Language |
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dc.contributor.advisor | Crocket, James H. | - |
dc.contributor.author | Gillespie, Randall T. | - |
dc.date.accessioned | 2015-07-29T15:17:30Z | - |
dc.date.available | 2015-07-29T15:17:30Z | - |
dc.date.issued | 1979-04 | - |
dc.identifier.uri | http://hdl.handle.net/11375/17818 | - |
dc.description.abstract | <p> The "F-Zone" is part of a migmatitic, radiometrically anomalous belt which forms the contact between a large granitic batholith and a region of homogeneous diatexite. Petrographic and geochemical analysis (including whole rock and rare-earth element analyses) of these three units has been carried out. Results indicate that the batholith was formed by partial fusion of sedimentary and volcanic material; the homogeneous diatexite arose in a similar way although fusion was less complete and; the migmatite incorporates material from both of these units. Late stage metasomatic-hydrothermal activity has concentrated uranium from the country rock in the migmatite zone.</p> | en_US |
dc.language.iso | en_US | en_US |
dc.subject | petrology, archean, migmatite, terrain, elements, fusion | en_US |
dc.title | Petrology and Geochemistry of an Archean Migmatite Terrain, Favourable Lake Area, Northwest Ontario | en_US |
dc.type | Thesis | en_US |
dc.contributor.department | Geology | en_US |
dc.description.degreetype | Thesis | en_US |
dc.description.degree | Bachelor of Science (BSc) | en_US |
Appears in Collections: | Bachelor theses |
Files in This Item:
File | Description | Size | Format | |
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Gillespie_Randall_T._1979Apr_Bachelors..pdf | 2.77 MB | Adobe PDF | View/Open |
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