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Experimental work bearing on the origin of hydrous nickel-magnesium silicate minerals.

Although the special study of the present work is an experimental investigation or the mineralogy, mode and conditions of formation of the hydrous nickel-magnesium silicates, often collectively referred to as garnierite, that characterize all nickel silicate deposits, it is felt that a brief description of the broader features and field relationships of the better-known nickel silicate deposits of the world would be an appropriate introduction to this subject.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.110141
Date January 1954
CreatorsMueller, George. V.
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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