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TitlePrecambrian bedrock geology, Boothia Peninsula, Nunavut, NTS 57-F and parts of 57-C, D, E, G and 67-D, E, H
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LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorGeological Survey of Canada
SourceGeological Survey of Canada, Canadian Geoscience Map 430, 2023, 1 sheet, https://doi.org/10.4095/331417 Open Access logo Open Access
LinksCollection de données de géologie de surface
Image
Year2023
PublisherNatural Resources Canada
Documentserial
Lang.English
Maps1 map
Map Info.geological, bedrock, 1:250,000
ProjectionUniversal Transverse Mercator Projection, UTM zone 15N
Mediadigital; on-line
File formatreadme
File formatpdf (Adobe® Reader®); rtf; pdf
ProvinceNunavut
NTS57F; 57C; 57D; 57E; 57G; 67D; 67E; 67H
AreaBoothia Peninsula
Lat/Long WENS -97.0000 -91.0000 71.5000 69.5000
Subjectsgeneral geology; Science and Technology; bedrock geology; Precambrian
Illustrationslocation maps; index maps
ProgramGEM2: Geo-mapping for Energy and Minerals Rae Province, Boothia-Somerset
Released2023 06 29
AbstractThis new map of the Precambrian geology of Boothia Peninsula, Nunavut, is a key tool to strengthen the geoscience knowledge base of north-central Nunavut, and presents a significant update to knowledge acquired in 1962 (Blackadar,1967) and 1986-1990 (Frisch, 2011). Through modern-concept bedrock mapping in 2017 and 2018 and supported by high-resolution geophysical and geochronological data sets, this map portrays in colours the location of at least 18 different crustal components that are distinguished on the basis of composition, mineral assemblage, and/or age. Several generations of folds and fabrics are portrayed (line types), with zones of more intense and localized high strain (shear zones) also shown (red). The new knowledge highlights a complex polydeformed terrane that is distinct from rocks to the south and southeast, and shows that mineral exploration strategies for other parts of Nunavut may not be transferable to the Boothia Peninsula - Somerset Island region.
Summary(Plain Language Summary, not published)
This new map of the Precambrian geology of Boothia Peninsula, Nunavut, is a key tool to strengthen the geoscience knowledge base of north-central Nunavut, and presents a significant update to knowledge acquired in 1962 (Blackadar,1967) and 1986-1990 (Frisch, 2011). Through modern-concept bedrock mapping in 2017 and 2018 and supported by high-resolution geophysical and geochronological data sets, this map portrays in colours the location of at least 18 different crustal components that are distinguished on the basis of composition, mineral assemblage, and/or age. Several generations of folds and fabrics are portrayed (line types), with zones of more intense and localized high strain (shear zones) also shown (red). The new knowledge highlights a complex polydeformed terrane that is distinct from rocks to the south and southeast, and shows that mineral exploration strategies for other parts of Nunavut may not be transferable to the Boothia Peninsula - Somerset Island region.
GEOSCAN ID331417

 
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