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A mineralogical study of pyrochlore and betafite.

Pyrochlore has been found in many localities and promises to be an important source of niobium. Betafite is also widespread in occurrence and has been mined intermittently in Madagascar as a minor uranium ore; in other localities it does not seem to occur in economic quantities. Although several independent studies of betafite and pyrochlore have been undertaken, the relationship of the one mineral to the other is not clear. The X-ray powder patterns of pyrochlore and ignited betafite are very similar although usually not identical. However, the chemical compositions are quite different.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.111783
Date January 1959
CreatorsHogarth, Donald. D.
ContributorsStevenson, J. (Supervisor)
PublisherMcGill University
Source SetsLibrary and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada
LanguageEnglish
Detected LanguageEnglish
TypeElectronic Thesis or Dissertation
Formatapplication/pdf
CoverageDoctor of Philosophy. (Department of Earth Sciences.)
RightsAll items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.
Relationalephsysno: NNNNNNNNN, Theses scanned by McGill Library.

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