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Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/16786
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DC FieldValueLanguage
dc.contributor.advisorSchwarcz, H.P-
dc.contributor.advisorCrocket, J.H.-
dc.contributor.authorBurnie, Stephen W.-
dc.date.accessioned2015-03-03T15:30:03Z-
dc.date.available2015-03-03T15:30:03Z-
dc.date.issued1970-12-
dc.identifier.urihttp://hdl.handle.net/11375/16786-
dc.description.abstractOre specimens from the cupriferous zone of the basal Nonesuch shale at the White Pine Mine were analysed for sulphur isotopes, carbon and sulphide contents and boron. The results of the analyses were discussed in relation to a biogenic-syngenetic mineralization process for the ore body. A model, based on the δS³⁴sulphide frequency distribution, was developed to determine the δS³⁴ sulphate value of the lower Nonesuch paleoenvironment. A transmitted light microscopic examination of chlorite was undertaken in order to present a more complete picture of this proposed source for copper in the cupriferous zone of the Nonesuch shale.en_US
dc.language.isoenen_US
dc.subjectore specimensen_US
dc.subjectWhite Pine Mineen_US
dc.subjectisotopesen_US
dc.subjectcarbonen_US
dc.subjectsulphuren_US
dc.subjectboronen_US
dc.subjectsulphideen_US
dc.titleSulphur Isotopes in the White Pine Mine, Ontonagon County, Michiganen_US
dc.typeThesisen_US
dc.contributor.departmentGeologyen_US
dc.description.degreetypeThesisen_US
dc.description.degreeMaster of Science (MSc)en_US
Appears in Collections:Open Access Dissertations and Theses

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