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The geology of the Forsyth and associated magnetite deposits, Hull Township, province of Quebec.

The rapid depletion of iron ore reserves in the Lake Superior region, coupled with increased blast furnace efficiencies resulting from the use of high grade iron ore concentrates, has created considerable interest in the development of low grade iron deposits throughout North America. As a result, the low grade magnetite deposits of the "Grenville" region of eastern Ontario and western Quebec have received considerable attention, and several large deposits such as the Marmora and Hilton mines have recently been brought into production. With this in mind, the writer was commissioned by Hull Iron Mines, Ltd., of Montreal to investigate a group of small magnetite deposits north of Hull, Quebec, which they are presently developing.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.111815
Date January 1959
CreatorsMachamer, Jerome. F.
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
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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