LEADER	03091nem a2200637 c 4500
001	129-288209
007	cr
008	2020 eng
034			|a 65.5000 -62.1667 65.5000 -64.1333 66.1667 -64.1333 66.1667 -62.0000 65.5000 -62.1667
041			|a eng
100			|a Sanborn-Barrie, M  |4 aut
245			|a Geology, Touak Fiord, Nunavut
250			|a prelim.
260			|b Natural Resources Canada  |c 2020
336			|b sti
338			|b nc
490			|a GEM: Geo-mapping for Energy and Minerals
520			|a Cumberland Peninsula, eastern Baffin Island, is an underexplored, frontier region with significant diamond and base- and precious-metal potential. Plutonic rocks of tonalitic to quartz dioritic composition across southern Cumberland Peninsula form the structural basement to supracrustal rocks that dominate its northern part. Tonalitic rocks are variably foliated to gneissic with preliminary Archean ages of ca. 2.77 Ga. Supracrustal rocks occurring as isolated strands in the south are inferred to be Archean. Extensive metasedimentary cover rocks of the Hoare Bay Group in the north include silicate- and oxide-facies iron-formation, chert, graphitic-pyritiferous shale, minor quartzite, and marble, with widespread psammite-semipelite turbidite. At several localities, mafic to ultramafic volcanic rocks preserve primary textures supporting both flow and pyroclastic origin. Additional mafic panels of uncertain origin are widespread. The Hoare Bay Group contains similar rock types and apparent stratigraphic associations as observed in the Paleoproterozoic Piling Group of central Baffin Island.
650			|a Bedrock Geology
650			|a Igneous Rocks
650			|a Plutonic Rocks
650			|a Metamorphic Rocks
650			|a Granites
650			|a Anorthosites
650			|a Gneisses
650			|a Pegmatites
650			|a Diorites
650			|a Tonalites
650			|a Volcanic Rocks
650			|a Sedimentary Rocks
650			|a Shales
650			|a Arenites
650			|a Komatiites
650			|a Granodiorites
650			|a Gabbros
650			|a Deformation
650			|a Structural Features
650			|a Faults
650			|a Folds
650			|a Metamorphism
650			|a Archean
650			|a Hoare Bay Group
650			|a Qikiqtarjuaq Plutonic Suite
650			|a Nunavut
650			|a Touak Fiord
650			|a Cumberland Peninsula
650			|a Baffin Island
655			|a Atlas  |2 gnd-content
700			|a Young, M  |4 aut
700			|a Whalen, J  |4 aut
700			|a James, D  |4 aut
700			|a St-Onge, M R  |4 aut
773	0	8	|g Geological Survey of Canada
856	4	0	|q text/html  |3 Link zur Ressource  |u https://geoscan.nrcan.gc.ca/starweb/geoscan/servlet.starweb?path=geoscan/fulle.web&search1=R=288209
856			|q text/html  |3 Multiple Metals - Cumberland Peninsula (Baffin Island, Nunavut), project number: MGM007 (latest publications):   |u https://geoscan.nrcan.gc.ca/starweb/geoscan/servlet.starweb?path=geoscan/shorte.web&search1=PROJECT=MGM007
980			|a 288209  |b 129  |c sid-129-col-geoscan

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author	Sanborn-Barrie, M, Young, M, Whalen, J, James, D, St-Onge, M R
author_facet	Sanborn-Barrie, M, Young, M, Whalen, J, James, D, St-Onge, M R
author_role	aut, aut, aut, aut, aut
author_sort	Sanborn-Barrie, M
author_variant	m s b msb, m y my, j w jw, d j dj, m r s o mrs mrso
building	Library A
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container_reference	Geological Survey of Canada
contents	Cumberland Peninsula, eastern Baffin Island, is an underexplored, frontier region with significant diamond and base- and precious-metal potential. Plutonic rocks of tonalitic to quartz dioritic composition across southern Cumberland Peninsula form the structural basement to supracrustal rocks that dominate its northern part. Tonalitic rocks are variably foliated to gneissic with preliminary Archean ages of ca. 2.77 Ga. Supracrustal rocks occurring as isolated strands in the south are inferred to be Archean. Extensive metasedimentary cover rocks of the Hoare Bay Group in the north include silicate- and oxide-facies iron-formation, chert, graphitic-pyritiferous shale, minor quartzite, and marble, with widespread psammite-semipelite turbidite. At several localities, mafic to ultramafic volcanic rocks preserve primary textures supporting both flow and pyroclastic origin. Additional mafic panels of uncertain origin are widespread. The Hoare Bay Group contains similar rock types and apparent stratigraphic associations as observed in the Paleoproterozoic Piling Group of central Baffin Island.
edition	prelim.
facet_avail	Online
format	eBook, StillImage
format_access_txtF_mv	Map
format_de105	Ebook, Map
format_de14	Map
format_de15	Map
format_detail_txtF_mv	map-online-monograph-independent
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format_finc	Book, E-Book, Visual Media
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format_strict_txtF_mv	Map, Website
genre	Atlas gnd-content
genre_facet	Atlas
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hierarchy_parent_title
hierarchy_sequence	Geological Survey of Canada
hierarchy_top_id
hierarchy_top_title
id	129-288209
illustrated	Not Illustrated
imprint	Natural Resources Canada, 2020
imprint_str_mv	Natural Resources Canada, 2020
institution	FID-MONTAN-DE-105
is_hierarchy_id
is_hierarchy_title
language	English
last_indexed	2024-01-31T13:31:24.669Z
match_str	sanbornbarrie2020geologytouakfiordnunavut
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publishDate	2020
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publisher	Natural Resources Canada
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record_id	288209
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series2	GEM: Geo-mapping for Energy and Minerals
source_id	129
spelling	Sanborn-Barrie, M aut, Geology, Touak Fiord, Nunavut, prelim., Natural Resources Canada 2020, sti, nc, GEM: Geo-mapping for Energy and Minerals, Cumberland Peninsula, eastern Baffin Island, is an underexplored, frontier region with significant diamond and base- and precious-metal potential. Plutonic rocks of tonalitic to quartz dioritic composition across southern Cumberland Peninsula form the structural basement to supracrustal rocks that dominate its northern part. Tonalitic rocks are variably foliated to gneissic with preliminary Archean ages of ca. 2.77 Ga. Supracrustal rocks occurring as isolated strands in the south are inferred to be Archean. Extensive metasedimentary cover rocks of the Hoare Bay Group in the north include silicate- and oxide-facies iron-formation, chert, graphitic-pyritiferous shale, minor quartzite, and marble, with widespread psammite-semipelite turbidite. At several localities, mafic to ultramafic volcanic rocks preserve primary textures supporting both flow and pyroclastic origin. Additional mafic panels of uncertain origin are widespread. The Hoare Bay Group contains similar rock types and apparent stratigraphic associations as observed in the Paleoproterozoic Piling Group of central Baffin Island., Bedrock Geology, Igneous Rocks, Plutonic Rocks, Metamorphic Rocks, Granites, Anorthosites, Gneisses, Pegmatites, Diorites, Tonalites, Volcanic Rocks, Sedimentary Rocks, Shales, Arenites, Komatiites, Granodiorites, Gabbros, Deformation, Structural Features, Faults, Folds, Metamorphism, Archean, Hoare Bay Group, Qikiqtarjuaq Plutonic Suite, Nunavut, Touak Fiord, Cumberland Peninsula, Baffin Island, Atlas gnd-content, Young, M aut, Whalen, J aut, James, D aut, St-Onge, M R aut, Geological Survey of Canada, text/html Link zur Ressource https://geoscan.nrcan.gc.ca/starweb/geoscan/servlet.starweb?path=geoscan/fulle.web&search1=R=288209, text/html Multiple Metals - Cumberland Peninsula (Baffin Island, Nunavut), project number: MGM007 (latest publications): https://geoscan.nrcan.gc.ca/starweb/geoscan/servlet.starweb?path=geoscan/shorte.web&search1=PROJECT=MGM007
spellingShingle	Sanborn-Barrie, M, Young, M, Whalen, J, James, D, St-Onge, M R, Geology, Touak Fiord, Nunavut, Cumberland Peninsula, eastern Baffin Island, is an underexplored, frontier region with significant diamond and base- and precious-metal potential. Plutonic rocks of tonalitic to quartz dioritic composition across southern Cumberland Peninsula form the structural basement to supracrustal rocks that dominate its northern part. Tonalitic rocks are variably foliated to gneissic with preliminary Archean ages of ca. 2.77 Ga. Supracrustal rocks occurring as isolated strands in the south are inferred to be Archean. Extensive metasedimentary cover rocks of the Hoare Bay Group in the north include silicate- and oxide-facies iron-formation, chert, graphitic-pyritiferous shale, minor quartzite, and marble, with widespread psammite-semipelite turbidite. At several localities, mafic to ultramafic volcanic rocks preserve primary textures supporting both flow and pyroclastic origin. Additional mafic panels of uncertain origin are widespread. The Hoare Bay Group contains similar rock types and apparent stratigraphic associations as observed in the Paleoproterozoic Piling Group of central Baffin Island., Bedrock Geology, Igneous Rocks, Plutonic Rocks, Metamorphic Rocks, Granites, Anorthosites, Gneisses, Pegmatites, Diorites, Tonalites, Volcanic Rocks, Sedimentary Rocks, Shales, Arenites, Komatiites, Granodiorites, Gabbros, Deformation, Structural Features, Faults, Folds, Metamorphism, Archean, Hoare Bay Group, Qikiqtarjuaq Plutonic Suite, Nunavut, Touak Fiord, Cumberland Peninsula, Baffin Island, Atlas
title	Geology, Touak Fiord, Nunavut
title_auth	Geology, Touak Fiord, Nunavut
title_full	Geology, Touak Fiord, Nunavut
title_fullStr	Geology, Touak Fiord, Nunavut
title_full_unstemmed	Geology, Touak Fiord, Nunavut
title_in_hierarchy
title_short	Geology, Touak Fiord, Nunavut
title_sort	geology touak fiord nunavut
title_unstemmed	Geology, Touak Fiord, Nunavut
topic	Bedrock Geology, Igneous Rocks, Plutonic Rocks, Metamorphic Rocks, Granites, Anorthosites, Gneisses, Pegmatites, Diorites, Tonalites, Volcanic Rocks, Sedimentary Rocks, Shales, Arenites, Komatiites, Granodiorites, Gabbros, Deformation, Structural Features, Faults, Folds, Metamorphism, Archean, Hoare Bay Group, Qikiqtarjuaq Plutonic Suite, Nunavut, Touak Fiord, Cumberland Peninsula, Baffin Island, Atlas
topic_facet	Bedrock Geology, Igneous Rocks, Plutonic Rocks, Metamorphic Rocks, Granites, Anorthosites, Gneisses, Pegmatites, Diorites, Tonalites, Volcanic Rocks, Sedimentary Rocks, Shales, Arenites, Komatiites, Granodiorites, Gabbros, Deformation, Structural Features, Faults, Folds, Metamorphism, Archean, Hoare Bay Group, Qikiqtarjuaq Plutonic Suite, Nunavut, Touak Fiord, Cumberland Peninsula, Baffin Island, Atlas
url	https://geoscan.nrcan.gc.ca/starweb/geoscan/servlet.starweb?path=geoscan/fulle.web&search1=R=288209