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TitleCurrent Research, Part C, Canadian Shield / Recherches En Cours, Partie C, Bouclier Canadien
LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorGeological Survey of Canada
SourceGeological Survey of Canada, Paper no. 91-1C, 1991, 205 pages, Open Access logo Open Access
Lang.English; French
Mediapaper; on-line; digital
RelatedThis publication contains the following publications
File formatpdf
ProvinceQuebec; Ontario; Saskatchewan; Manitoba; Northwest Territories; Nunavut
NTS24; 25; 31; 32; 34; 35; 36; 41; 45; 46; 55; 56; 58; 63; 66; 68; 74; 86; 87; 97
AreaVal-d'Or; Kirkland Lake; Larder Lake; Athabasca; Noranda; Elliot Lake; Ungava Peninsula; Bluenose Lake; Lake Ontario; Lake Huron; Lake Erie; Saint Jovite; Contwoyto Lake; Hudson Bay; Abitibi; Matagami; Chapais; Whitehills; Tehek; Flin Flon; Somerset Island; Prince of Wales Island; Lac Watts; Purtuniq; Coats Island
Lat/Long WENS-128.0000 -64.0000 76.0000 44.0000
Subjectseconomic geology; geochemistry; metallic minerals; sedimentology; tectonics; geophysics; igneous and metamorphic petrology; mineralogy; structural geology; surficial geology/geomorphology; igneous rocks; sedimentary rocks; lithology; geochemical analyses; structural features; tectonic elements; tectonic zones; deformation; metamorphism; sulphides; glacial deposits; geophysical surveys; Churchill Province; Grenville Province; Superior Province; Abitibi Belt; Canadian Shield; Proterozoic; Precambrian; Phanerozoic; Paleozoic; Mesozoic; Cenozoic
Illustrationscharts; tables; photomicrographs; seismic profiles; cross-sections; photographs; sketch maps; stereonets
Released1991 02 01; 2013 08 13
AbstractEast of Val d'Or, gneisses with a dominant mafic and a widespread, minor ultramafic component can be followed into the Grenville Province some 80 km eastward from the Grenville Front. These gneisses are oriented east-west. This orientation may be inherited from Archean structures. Other large areas are underlain by gneisses of intermediate to Je/sic composition with widespread subor

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