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Iron silicate equilibria in the Cape Smith Belt, New Quebec.

This thesis is a study of phase equilibria among iron-rich silicate minerals in the metamorphic iron formations in the Cape Smith Belt, New Quebec, and is based on the chemical analyses of eight iron-rich silicate minerals. Mineral assemblages investigated include: grunerite-stilpnomelane, grunerite-stilpnomelane-almandite-biotite, stilpnomelane-minnesotaite-iron chlorite, all with quartz, magnetite, and calcite. Their stability relationships in the system FeO-MgO-Fe203-Al203-Si02-H20, during metamorphism are discussed.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.113665
Date January 1962
CreatorsHashimoto, Tsutomu.
ContributorsEakins, P. (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
CoverageMaster of Science. (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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