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.
Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.113665 |
Date | January 1962 |
Creators | Hashimoto, Tsutomu. |
Contributors | Eakins, P. (Supervisor) |
Publisher | McGill University |
Source Sets | Library and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada |
Language | English |
Detected Language | English |
Type | Electronic Thesis or Dissertation |
Format | application/pdf |
Coverage | Master of Science. (Department of Earth Sciences.) |
Rights | All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. |
Relation | alephsysno: NNNNNNNNN, Theses scanned by McGill Library. |
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