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TitleGeology, Barrow River, Melville Peninsula, Nunavut, NTS 46-O and 46-P
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LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorCorrigan, DORCID logo; Nadeau, L; Brouillette, P; Wodicka, NORCID logo; Berman, R GORCID logo; Houlé, M G
SourceGeological Survey of Canada, Canadian Geoscience Map 236, 2020, 1 sheet, https://doi.org/10.4095/297366 Open Access logo Open Access
Image
Year2020
PublisherNatural Resources Canada
Documentserial
Lang.English
Maps1 map
Map Info.geological, stratigraphic, structural, 1:150,000
ProjectionUniversal Transverse Mercator Projection, UTM zone 17 (NAD83)
Mediadigital; on-line
RelatedNRCan photo(s) in this publication
File formatreadme
File formatpdf; rtf; gdb (ESRI® ArcGIS(TM) v.10.x); shp (ESRI® ArcGIS(TM) v.10.x); xml (ESRI® ArcGIS(TM) v.10.x); xls (Microsoft® Excel®); mxd (ESRI® ArcGIS(TM) v.10.x)
ProvinceNunavut
NTS46O; 46P
AreaBarrow River; Melville Peninsula
Lat/Long WENS -84.0000 -81.1667 68.0000 67.0000
Subjectsregional geology; structural geology; stratigraphy; economic geology; geochronology; mineralogy; tectonics; Nature and Environment; Science and Technology; bedrock geology; basement geology; lithology; igneous rocks; volcanic rocks; anorthosites; rhyolites; lava flows; intrusive rocks; granites; aplites; pegmatites; gabbros; granodiorites; leucogabbros; diorites; monzo-granites; metamorphic rocks; metavolcanic rocks; gneisses; metasedimentary rocks; metagreywackes; metapelites; marbles; metapsammites; quartzites; migmatites; granulites; amphibolites; metagabbros; sedimentary rocks; dolomites; limestones; pelites; marls; iron formations; structural features; faults; faults, normal; faults, slip; faults, thrust; folds; folds, overturned; antiforms; synforms; bedding planes; tectonic history; folding; faulting; rifting; metamorphism; emplacement; magmatism; intrusions; dykes; crustal uplift; mineral occurrences; lead; zinc; silver; gold; nickel; copper; uranium; molybdenum; tungsten; arsenic; textures; foliation; gneissosity; lineations; crenulations; radiometric dating; uranium lead dating; zircon dates; Archean; Neoproterozoic; Paleoproterozoic; Penrhyn Group; Franklin Dykes; Mackenzie Dykes; Longstaff Bluff Formation; Astarte River Formation; Flint Lake Formation; Dewar Lakes Formation; Piling Group; geological contacts; Phanerozoic; Paleozoic; Silurian; Ordovician; Proterozoic; Precambrian
Illustrationslocation maps; index maps; photographs; tables; diagrams
ProgramGEM2: Geo-mapping for Energy and Minerals Hudson/Ungava Project Management
Released2020 07 17
AbstractThe Barrow River bedrock geology map is the product of targeted mapping carried out during the summer of 2010, enhanced by radiometric age-dating as well as high-resolution aeromagnetic and radiometric surveys completed over previously published geological maps of the Paleoproterozoic Penrhyn Group and its Archean basement in southeastern Melville Peninsula, Nunavut. The high-resolution aeromagnetic survey was utilized to project lithological boundaries beneath Quaternary cover. The map shows complex basement-cover relationships characterized by multiple generations of thrusting and folding in a thick-skinned tectonic regime, followed by dextral transpression along the southern edge of the Penrhyn Group. A late-Archean tectonometamorphic event is recorded by ca. 2.55 Ga monazite in basement gneiss. Onset of rifting prior to deposition of the Penrhyn Group may be indicated by the emplacement of a bimodal suite of granite and leucogabbro-anorthosite at ca. 2.02 Ga. Penrhyn Group units are tentatively correlated with the Piling Group on Baffin Island.
Summary(Plain Language Summary, not published)
This map is a synthesis of recent field observations, radiometric age-dating, high-resolution aeromagnetic surveys and previously published geological maps of the Paleoproterozoic-age Penrhyn Group and its Archean basement in southeastern Melville Peninsula, Nunavut. This new work stems from the Melville Peninsula Multiple Metal project initiated in 2009 under the auspices of the Geo-Mapping for Energy and Minerals (GEM-1) program. Targeted field work was initiated in 2009, followed by more systematic coverage by ground traverses in the summer 2010. The map shows complex basement-cover relationships characterized by multiple generations of thrusting and folding in a thick-skinned tectonic regime, followed by dextral transpression. A late-Archean tectonometamorphic event is recorded by ca. 2.55 Ga monazite in basement gneiss. Onset of rifting prior to deposition of the Penrhyn Group may be indicated by the emplacement of a bimodal suite of granite and leucogabbro-anorthosite at ca. 2.02 Ga. Penrhyn Group units are tentatively correlated with the Piling Group on Baffin Island.
GEOSCAN ID297366

 
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