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The nature of the olivine - spinel transition in the Mg2SiO4-Fe2SiO4 system and its geophysical implications.

Thesis. 1976. Ph.D.--Massachusetts Institute of Technology. Dept. of Earth and Planetary Sciences. / Microfiche copy available in Archives and Science. / Vita. / Bibliography: leaves 315-334. / Ph.D.

Identiferoai:union.ndltd.org:MIT/oai:dspace.mit.edu:1721.1/59019
Date January 1976
CreatorsSung, Chien-Min, 1947-
ContributorsRoger G. Burns., Massachusetts Institute of Technology. Department of Earth and Planetary Sciences, Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
PublisherMassachusetts Institute of Technology
Source SetsM.I.T. Theses and Dissertation
LanguageEnglish
Detected LanguageEnglish
TypeThesis
Format337, [33] leaves, [50] p., application/pdf
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., http://dspace.mit.edu/handle/1721.1/7582

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