| Title | Current Research, Part C, Canadian Shield / Recherches En Cours, Partie C, Bouclier Canadien |
| Download | Downloads |
| |
| 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, Paper no. 91-1C, 1991, 205 pages, https://doi.org/10.4095/132553  Open Access |
| Image |  |
| Year | 1991 |
| Document | serial |
| Lang. | English; French |
| Media | paper; on-line; digital |
| Related | This publication contains the following
publications |
| File format | pdf |
| Province | Quebec; Ontario; Saskatchewan; Manitoba; Northwest Territories; Nunavut |
| NTS | 24; 25; 31; 32; 34; 35; 36; 41; 45; 46; 55; 56; 58; 63; 66; 68; 74; 86; 87; 97 |
| Area | Val-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 |
| Subjects | economic 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 |
| Illustrations | charts; tables; photomicrographs; seismic profiles; cross-sections; photographs; sketch maps; stereonets |
| Released | 1991 02 01; 2013 08 13 |
| Abstract | East 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 |
| GEOSCAN ID | 132553 |
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