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The geology of Malartic Gold Fields mine, Halet, Quebec.

The mine is located 6 miles east of the Town of Malartic, and is about 300 miles northwest of Montreal. A belt of altered peridotite about 2,500' wide trends southeasterly across the property. An embayment of talc-chlorite rock branches from the Cadillac fault, which forms the north contact of the peridotite, into the peridotite belt in a southeasterly direction. [...]

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.119042
Date January 1954
CreatorsBlack, Philip Thomas.
ContributorsGill, 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 Geological 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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