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Growth of sulphides in black shales.

Sulphides can be divided into two major groups, those which are of hydrothermal origin and those which are of sedimentary origin. The sulphides of sedimentary origin are found in greatest abundance in bituminous rocks and it is these sulphides that have been investigated in the present work. A study of the sedimentary sulphides is of special importance with respect to ore deposits because the various chemical and geological conditions present at the time of deposition, compaction, and metamorphism of the sediment can have a profound effect on the mineral associations and metal concentrations of the rocks.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.111780
Date January 1959
CreatorsHay, Robert. E.
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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