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Geology of Knob Lake Ridge, Schefferville, Quebec.

The Knob Lake Ridge is located near Schefferville townsite, three hundred and seventy miles north of Seven Islands; the Knob Lake Ridge defines the New-Quebec-Newfoundland-Labrador boundary adjacent to the critical ore zone. The Labrador trough represents a structural depression seven hundred miles long and twenty to sixty miles in width running southeast-northwest and extending south from the Payne River situated at the 60° parallel on the western shores of Ungava Bay to the fifty first degree parallel. This trough represents a geosyncline that was partially filled by a succession of sedimentary strata.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.115242
Date January 1963
CreatorsSeguin, Maurice.
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
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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