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http://hdl.handle.net/11375/19214
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DC Field | Value | Language |
---|---|---|
dc.contributor.advisor | Kramer, J. R. | - |
dc.contributor.author | Malcolmson, Sarah | - |
dc.date.accessioned | 2016-05-05T13:41:05Z | - |
dc.date.available | 2016-05-05T13:41:05Z | - |
dc.date.issued | 1995-04 | - |
dc.identifier.uri | http://hdl.handle.net/11375/19214 | - |
dc.description.abstract | <P> The occurrence of silver in galena, chalcopyrite, sphalerite, and pyrite as well as tailings from Cart Lake, Cobalt Ontario were investigated to compare with the undetectable ( <10^-11 g/g) Ag found in runoff water from the Cobalt area. </p> <p> Silver was detected at very low levels: 0.012 wt% ± 0.009 wt%, 0.015 wt% ± 0.01 wt%, and 0.0062 wt% ±0.02 wt% for pyrite, galena and chalcopyrite, respectively. </p> <p> Attempts to characterize the mineralogical associations of silver were not successful. The silver sequence of pyrite> galena> chalcopyrite is contrary to results from other studies. This may be due to the maximum thermal stabilities of the minerals in relation to the ions available for replacement. </p> | en_US |
dc.language.iso | en | en_US |
dc.subject | Metal Sulphides | en_US |
dc.subject | cobalt | en_US |
dc.subject | Silver Substitution | en_US |
dc.subject | galena | en_US |
dc.subject | chalcopyrite | en_US |
dc.subject | sphalerite | en_US |
dc.title | Silver Substitution into Common Metal Sulphides from Cobalt, Ontario | 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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Malcolmson_Sarah_1995_Bachelors.pdf | 7.68 MB | Adobe PDF | View/Open |
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