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A method for determining the solubility of sulphides.

Many orebodies have been formed in low temperature environments, distant from any known source and beyond the influence of ground water. These facts imply that ore metals travel in some way from a source to the places where they are found. Various theories have been put forward which purport to explain how this may happen. Because metals and their common silicates and sulphides are, with a few exceptions, volatile only at temperatures considerably above the temperatures at which epithermal deposits are thought to form, most theories postulate the presence of water to act as a moving flux in which the ore constituents are carried along.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.111289
Date January 1957
CreatorsRelly, Bruce. H.
ContributorsSaull, V. (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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