Geology of Cape Makkovik Peninsula, Aillik Labrador

This thesis is concerned with the most promising molybdenite-rich area on the north coast of Labrador, Cape Makkovik peninsula. The area, although only 6 square miles in size, is part of the Labrador Uranium Province and its geology is similar to the Beaverlodge and Great Bear Lake camps in the west...

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Main Author: King, A. F.
Format: Thesis
Language:English
Published: Memorial University of Newfoundland 1963
Subjects:
Online Access:https://research.library.mun.ca/6914/
https://research.library.mun.ca/6914/1/AFKing.pdf
https://research.library.mun.ca/6914/3/AFKing.pdf
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spelling ftmemorialuniv:oai:research.library.mun.ca:6914 2023-10-01T03:56:11+02:00 Geology of Cape Makkovik Peninsula, Aillik Labrador King, A. F. 1963 application/pdf https://research.library.mun.ca/6914/ https://research.library.mun.ca/6914/1/AFKing.pdf https://research.library.mun.ca/6914/3/AFKing.pdf en eng Memorial University of Newfoundland https://research.library.mun.ca/6914/1/AFKing.pdf https://research.library.mun.ca/6914/3/AFKing.pdf King, A. F. <https://research.library.mun.ca/view/creator_az/King=3AA=2E_F=2E=3A=3A.html> (1963) Geology of Cape Makkovik Peninsula, Aillik Labrador. Masters thesis, Memorial University of Newfoundland. thesis_license Thesis NonPeerReviewed 1963 ftmemorialuniv 2023-09-03T06:46:07Z This thesis is concerned with the most promising molybdenite-rich area on the north coast of Labrador, Cape Makkovik peninsula. The area, although only 6 square miles in size, is part of the Labrador Uranium Province and its geology is similar to the Beaverlodge and Great Bear Lake camps in the western part of the Canadian Shield. -- In a reconnaissance along the Labrador coast in 1900, Daly referred to the glaciated peninsula as "a veritable museum of rock types". The map-area is underlain by an assemblage of folded metamorphosed quartzitic and amphibolitic rocks of Precambrian age which have been termed the Aillik Group. The degree of metamorphism has been largely dependent upon the original character of the rock and upon tectonic stresses which prevailed during deformation. A great number and variety of intrusive rocks ranging in composition from "amazonite" pegmatite to lamprophyre have been intruded at different times along major joint sets. -- After detailed megascopic and microscopic study, parentage has been determined for those metamorphosed and metasomatized (potash-bearing) rocks which have retained some of their primary features. The relative ages of the igneous rocks have been determined and these observations, combined with radioactive age determinations, may possibly be a means of chronological correlation with dyke systems in other parts of Labrador. -- The thesis is illustrated by figures and plates, and by a coloured geological map on a scale of 1 inch to 500 feet. Thesis Great Bear Lake Makkovik Memorial University of Newfoundland: Research Repository Great Bear Lake ENVELOPE(-120.753,-120.753,65.834,65.834) Daly ENVELOPE(63.761,63.761,-67.513,-67.513) Makkovik ENVELOPE(-59.178,-59.178,55.087,55.087)
institution Open Polar
collection Memorial University of Newfoundland: Research Repository
op_collection_id ftmemorialuniv
language English
description This thesis is concerned with the most promising molybdenite-rich area on the north coast of Labrador, Cape Makkovik peninsula. The area, although only 6 square miles in size, is part of the Labrador Uranium Province and its geology is similar to the Beaverlodge and Great Bear Lake camps in the western part of the Canadian Shield. -- In a reconnaissance along the Labrador coast in 1900, Daly referred to the glaciated peninsula as "a veritable museum of rock types". The map-area is underlain by an assemblage of folded metamorphosed quartzitic and amphibolitic rocks of Precambrian age which have been termed the Aillik Group. The degree of metamorphism has been largely dependent upon the original character of the rock and upon tectonic stresses which prevailed during deformation. A great number and variety of intrusive rocks ranging in composition from "amazonite" pegmatite to lamprophyre have been intruded at different times along major joint sets. -- After detailed megascopic and microscopic study, parentage has been determined for those metamorphosed and metasomatized (potash-bearing) rocks which have retained some of their primary features. The relative ages of the igneous rocks have been determined and these observations, combined with radioactive age determinations, may possibly be a means of chronological correlation with dyke systems in other parts of Labrador. -- The thesis is illustrated by figures and plates, and by a coloured geological map on a scale of 1 inch to 500 feet.
format Thesis
author King, A. F.
spellingShingle King, A. F.
Geology of Cape Makkovik Peninsula, Aillik Labrador
author_facet King, A. F.
author_sort King, A. F.
title Geology of Cape Makkovik Peninsula, Aillik Labrador
title_short Geology of Cape Makkovik Peninsula, Aillik Labrador
title_full Geology of Cape Makkovik Peninsula, Aillik Labrador
title_fullStr Geology of Cape Makkovik Peninsula, Aillik Labrador
title_full_unstemmed Geology of Cape Makkovik Peninsula, Aillik Labrador
title_sort geology of cape makkovik peninsula, aillik labrador
publisher Memorial University of Newfoundland
publishDate 1963
url https://research.library.mun.ca/6914/
https://research.library.mun.ca/6914/1/AFKing.pdf
https://research.library.mun.ca/6914/3/AFKing.pdf
long_lat ENVELOPE(-120.753,-120.753,65.834,65.834)
ENVELOPE(63.761,63.761,-67.513,-67.513)
ENVELOPE(-59.178,-59.178,55.087,55.087)
geographic Great Bear Lake
Daly
Makkovik
geographic_facet Great Bear Lake
Daly
Makkovik
genre Great Bear Lake
Makkovik
genre_facet Great Bear Lake
Makkovik
op_relation https://research.library.mun.ca/6914/1/AFKing.pdf
https://research.library.mun.ca/6914/3/AFKing.pdf
King, A. F. <https://research.library.mun.ca/view/creator_az/King=3AA=2E_F=2E=3A=3A.html> (1963) Geology of Cape Makkovik Peninsula, Aillik Labrador. Masters thesis, Memorial University of Newfoundland.
op_rights thesis_license
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