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Isotopic systematics of ultramafic and mafic rocks of the Taitao ophiolite, southern Chile

dc.contributor.advisorWalker, Richard Jen_US
dc.contributor.authorSchulte, Ruth Frosten_US
dc.date.accessioned2007-06-22T05:31:57Z
dc.date.available2007-06-22T05:31:57Z
dc.date.issued2007-03-14
dc.identifier.urihttp://hdl.handle.net/1903/6705
dc.description.abstractA variety of ultramafic and mafic rocks from a well-mapped sampling of the ~6 Ma Taitao Ophiolite, Chile, have been examined. Calculated initial 187Os/188Os ratios of the peridotitic rocks range from 0.1168 to 0.1282. Similar ranges of Os isotopic compositions have been reported for abyssal peridotites, peridotites, and chromites from other ophiolites. A correlation between Mg # of primary olivine and Os isotopic compositions of whole rock peridotites suggests that the isotopic variability is due to variable extents of partial melting at ~1.5 Ga. This conclusion is also supported by a linear correlation between 187Re/188Os and 187Os/188Os. The ancient melting event requires that this km-scale block of the mantle remained isolated and unmixed within the convecting upper mantle for a period of ~1.5 Ga. The results are comparable to global observations of Os isotopic compositions in mid-ocean ridge basalts versus abyssal peridotites, but the geologic relations here are well-defined.en_US
dc.format.extent2714389 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleIsotopic systematics of ultramafic and mafic rocks of the Taitao ophiolite, southern Chileen_US
dc.typeThesisen_US
dc.contributor.publisherDigital Repository at the University of Marylanden_US
dc.contributor.publisherUniversity of Maryland (College Park, Md.)en_US
dc.contributor.departmentGeologyen_US
dc.subject.pqcontrolledGeochemistryen_US
dc.subject.pqcontrolledGeochemistryen_US
dc.subject.pquncontrolledisotope geochemistyen_US
dc.subject.pquncontrolledosmiumen_US
dc.subject.pquncontrolledophiolitesen_US
dc.subject.pquncontrolledconvecting upper mantleen_US
dc.subject.pquncontrolledchromitesen_US


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