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Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/17876
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DC FieldValueLanguage
dc.contributor.advisorShaw, D.M.-
dc.contributor.authorGoodale, Douglas H.-
dc.date.accessioned2015-08-06T21:36:39Z-
dc.date.available2015-08-06T21:36:39Z-
dc.date.issued1971-05-
dc.identifier.urihttp://hdl.handle.net/11375/17876-
dc.description.abstract<p> Precambrian iron formations from N.W. Ontario and Melville Peninsula, District of Franklin, were analyzed for Li and major elements. The N.W. Ontario samples contain little Li (0.46 to 5.88 ppm) but high percentages of mafic silicates (20 to 50%). The Melville Peninsula samples show the opposite, having higher Li (1.65 to 58.2 ppm) and lower silicate material (0.6 to 25.0%).</p> <p> Results from acetic acid leaching experiments show that part of the Li in the Melville irons may be removed, indicating Li to be present both by absorption and substitution.</p> <p> The higher Li abundances in the Melville Peninsula rocks may be attributed to the effect of later intrusive granites.</p>en_US
dc.language.isoen_USen_US
dc.subjectprecambrian, iron, material, lithiumen_US
dc.titleAn Investigation of Lithium Distribution in Certain Precambrian Iron Formationsen_US
dc.typeThesisen_US
dc.contributor.departmentGeologyen_US
dc.description.degreetypeThesisen_US
dc.description.degreeBachelor of Science (BSc)en_US
Appears in Collections:Bachelor theses

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