Title | Precambrian bedrock geology, Boothia Peninsula, Nunavut, NTS 57-F and parts of 57-C, D, E, G and 67-D, E, H |
Download | Downloads |
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Licence | Please note the adoption of the Open Government Licence - Canada
supersedes any previous licences. |
Author | Geological Survey of Canada |
Source | Geological Survey of Canada, Canadian Geoscience Map 430, 2023, 1 sheet, https://doi.org/10.4095/331417 Open Access |
Links | Collection de données de géologie de surface
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Image |  |
Year | 2023 |
Publisher | Natural Resources Canada |
Document | serial |
Lang. | English |
Maps | 1 map |
Map Info. | geological, bedrock, 1:250,000 |
Projection | Universal Transverse Mercator Projection, UTM zone 15N |
Media | digital; on-line |
File format | readme
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File format | pdf (Adobe® Reader®); rtf; pdf |
Province | Nunavut |
NTS | 57F; 57C; 57D; 57E; 57G; 67D; 67E; 67H |
Area | Boothia Peninsula |
Lat/Long WENS | -97.0000 -91.0000 71.5000 69.5000 |
Subjects | general geology; Science and Technology; bedrock geology; Precambrian |
Illustrations | location maps; index maps |
Program | GEM2: Geo-mapping for Energy and Minerals Rae Province, Boothia-Somerset |
Released | 2023 06 29 |
Abstract | 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. |
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 ID | 331417 |
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