Title | Detrital mineral provenance analyses from the Cretaceous McMurray Formation, Alberta and the Holocene Portneuf river delta, North Shore of Quebec |
Download | Downloads |
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Licence | Please note the adoption of the Open Government Licence - Canada
supersedes any previous licences. |
Author | Pe-Piper, G; Piper, D J W ; Blowick, A; Gomez Garcia, G; Wallace, K; Sangster, C |
Source | Geological Survey of Canada, Open File 8761, 2021, 391 pages, https://doi.org/10.4095/327838 Open Access |
Image |  |
Year | 2021 |
Publisher | Natural Resources Canada |
Document | open file |
Lang. | English |
Media | on-line; digital |
File format | readme
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File format | pdf; rtf; xlsx (Microsoft® Excel®) |
Province | Alberta; Quebec |
NTS | 22C/11; 73E; 73F; 73K; 73L; 73M; 73N; 74C; 74D; 74E; 74F; 74K; 74L; 74M; 74N; 75C; 75D; 83E; 83F; 83G; 83H; 83I; 83J; 83K; 83L; 83M; 83N; 83O; 83P; 84; 85A; 85B; 85C; 85D |
Area | Rivière Portneuf; Rivière du Sault aux Cochons; Fort McMurray; Fort McKay; Peace River |
Lat/Long WENS | -69.1000 -69.0500 48.7333 48.6333 |
Lat/Long WENS | -120.0000 -108.0000 61.0000 53.0000 |
Subjects | geochemistry; mineralogy; regional geology; sedimentology; surficial geology/geomorphology; Nature and Environment; Science and Technology; Holocene; Lower Cretaceous; Aptian; bedrock geology;
lithology; sedimentary rocks; deltaic sediments; sands; paleodrainage; provenance; isotopic studies; lead isotope ratios; feldspar; mineral assemblages; heavy mineral analyses; detrital minerals; petrographic analyses; electron microscope analyses;
clasts; McMurray Formation; Ancestral Sable River; Western Interior Seaway; Trans-Hudson Orogen; Grenville Province; Mohawk B-93 Well; Scotian Basin; Appalachian Province; alluvial sediments; Phanerozoic; Cenozoic; Quaternary; Mesozoic; Cretaceous;
Jurassic; Precambrian; Proterozoic |
Illustrations | tables; geoscientific sketch maps; photomicrographs; plots; pie charts; ternary diagrams; photographs; schematic representations; seismic profiles; profiles; stratigraphic charts; lithologic
sections; correlation sections; location maps; geochronological charts |
Program | Geoscience for New Energy Supply (GNES) Program Coordination |
Released | 2021 01 25 |
Abstract | The dispersion of sandy sediment by the early Cretaceous Sable River has been further investigated by detailed mineralogical study of (a) two samples from the Aptian McMurray Formation of Alberta and
(b) a Holocene deltaic deposit on the North Shore of the St Lawrence Estuary. Samples from Alberta were to test the hypothesis that Aptian diversion of the Sable River led to it flowing to the Western Interior Seaway, contributing sand to the
McMurray Formation. Pb-isotopes in K-feldspar show that most of the first cycle feldspars in the McMurray Formation were derived from the local Trans-Hudson Orogen. The heavy mineral assemblage, particularly the abundance of staurolite and paucity of
chromite, is different from that of the Sable River. The Holocene deltaic sand was analysed to identify distinctive heavy minerals from that part of the Grenville terrane. Garnets are similar to enigmatic garnets from the Jurassic of the Mohawk B-93
well, where Pb-isotopes on K-feldspar also suggest a Grenville source. Titania minerals with abundant quartz inclusions, known from both the Scotian Basin and the McMurray Formation, were not present in the Holocene sample and their provenance
significance remains enigmatic. |
Summary | (Plain Language Summary, not published) This Open File provides data on diagnostic minerals in sandstones that can be used for comparison with previous studies in the offshore Scotian Basin to
understand sources of sand to petroleum reservoir rocks. |
GEOSCAN ID | 327838 |
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