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dc.contributor.advisorTimothy L. Grove.en_US
dc.contributor.authorZervas, Deborah Aen_US
dc.date.accessioned2010-09-02T17:11:04Z
dc.date.available2010-09-02T17:11:04Z
dc.date.copyright1991en_US
dc.date.issued1991en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/58238
dc.descriptionThesis (M.S.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1991.en_US
dc.descriptionIncludes bibliographical references (leaves 13-15).en_US
dc.description.statementofresponsibilityby Deborah A. Zervas.en_US
dc.format.extent32 leavesen_US
dc.language.isoengen_US
dc.publisherMassachusetts Institute of Technologyen_US
dc.rightsM.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.en_US
dc.rights.urihttp://dspace.mit.edu/handle/1721.1/7582en_US
dc.subjectEarth, Atmospheric, and Planetary Sciencesen_US
dc.titleThe dependence on oxygen fugacity of nickel and cobalt partitioning between olivine and silicate melten_US
dc.typeThesisen_US
dc.description.degreeM.S.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
dc.identifier.oclc26176482en_US


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