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TitleDevonian of the Mackenzie
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LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorKabanov, PORCID logo
SourceSedimentary basins of northern Canada: contributions to a 1000 Ma geological journey and insight on resource potential; by Lavoie, DORCID logo (ed.); Dewing, KORCID logo (ed.); Geological Survey of Canada, Bulletin 609, 2022 p. 129-158, https://doi.org/10.4095/326094 Open Access logo Open Access
LinksErratum
Image
Year2022
PublisherNatural Resources Canada
Documentserial
Lang.English
Mediaon-line; digital
RelatedThis publication is contained in Sedimentary basins of northern Canada: contributions to a 1000 Ma geological journey and insight on resource potential
File formatpdf
ProvinceNorthwest Territories; Yukon
NTS96B/09; 96B/10; 96B/11; 96B/12; 96B/13; 96B/14; 96B/15; 96B/16; 96C/09; 96C/10; 96C/11; 96C/12; 96C/13; 96C/14; 96C/15; 96C/16; 96D; 96E/01; 96E/07; 96E/08; 96E/09; 96E/10; 96E/14; 96E/15; 96E/16; 96K; 96L; 96M; 96N; 106E; 106F; 106G; 106H; 106I; 106J; 106K; 106L; 106M; 106N; 106O; 106P
AreaMackenzie Valley; Mackenzie Mountains; Norman Wells; Colville Hills; Franklin Mountains; Richardson Mountains
Lat/Long WENS-136.0000 -124.0000 68.0000 64.5000
Subjectsregional geology; stratigraphy; paleontology; structural geology; tectonics; fossil fuels; economic geology; geochemistry; Science and Technology; Nature and Environment; sedimentary basins; systematic stratigraphy; stratigraphic nomenclature; stratigraphic analyses; stratigraphic correlations; tectonostratigraphic zones; lithostratigraphy; biostratigraphy; micropaleontology; microfossils; conodonts; fossil zones; depositional environment; depositional history; burial history; exploration wells; bedrock geology; lithology; sedimentary rocks; carbonates; limestones; dolostones; evaporites; anhydrite; shales; cherts; siltstones; sandstones; conglomerates; breccias; nodules; structural features; grabens; faults; petroleum resources; petroleum exploration; hydrocarbon potential; hydrocarbons; oil; gas; petroleum occurrence; thermal maturation; source rocks; tectonic setting; deformation; tectonic elements; paleogeography; continental margins; mineral deposits; barite; metals; polymetallic ores; strata-bound deposits; nickel; zinc; molybdenum; mineral exploration; mineral potential; mineral occurrences; disconformities; unconformities; x-ray fluorescence analyses; field relations; Lower Mississippian; Canadian Cordillera; Laramide Orogeny; Interior Plains; Peel Plain; Anderson Plain; Peel Plateau; Mackenzie Plain; Keele Arch; Keele Tectonic Zone; Norman Wells High; Richardson Trough; Peel-Mackenzie Platform; Ellesmerian Orogeny; Root Basin; Canol shale play; Norman Range Thrust Fault; Delorme Group; Arnica Formation; Landry Formation; Bear Rock Formation; Fort Norman Formation; Hume Formation; Clare Member; Road River Group; Horn River Group; Hare Indian Formation; Bell Creek Member; Bluefish Member; Francis Creek Member; Prohibition Creek Member; Ramparts Formation; Carcajou Member; Kee Scarp Member; Canol Formation; Dodo Canyon Member; Vermillion Creek Member; Imperial Formation; Canyon Member; Mirror Lake Member; Loon Creek Member; Jungle Ridge Member; Tuttle Formation; Ford Lake Formation; Camsell Formation; Headless Formation; Mount Baid Formation; Mount Kindle Formation; Peel Formation; Tatsieta Formation; Tsetso Formation; platinum group elements; Phanerozoic; Paleozoic; Carboniferous; Mississippian; Devonian
Illustrationsgeoscientific sketch maps; stratigraphic sections; cross-sections; stratigraphic charts; logs; biostratigraphic charts; correlation charts; profiles; tables
ProgramGEM2: Geo-mapping for Energy and Minerals Mackenzie Corridor Project Management
Released2022 12 20; 2023 09 14
AbstractThis paper reviews the Devonian-Lower Mississippian strata of NTS areas 106 and 96 lying within Geo-mapping for Energy and Minerals (GEM) Mackenzie project area and its vicinity. These strata are usually well in excess of 1 km in non-eroded sections, cropping out extensively in the Cordillera and occurring in the subsurface of adjacent Interior Plains. Major tectonostratigraphic assemblages are the latest Silurian-Eifelian platform carbonates and evaporites, the latest Eifelian-Frasnian basinal mudrocks with isolated carbonate banks bundled in the Horn River Group (HRG), and the thick coarsening-upward siliciclastic succession of Frasnian-Tournaisian age deposited in the distal setting of the Ellesmerian foreland basin. A major total petroleum system of the HRG defines the economic prospectivity of Devonian strata. Review of the lithostratigraphic nomenclature is supplemented with highlights on HRG depositional environments, patterns of thermal maturity, disconformities, and sedimentary cycles in platform carbonates.
Summary(Plain Language Summary, not published)
This chapter reviews the Devonian-Lower Mississippian strata of NTS areas 106 and 96 lying within GEM Mackenzie Project area and its vicinity. These strata are usually well in excess of 1 km in non-eroded sections, cropping out extensively in the Cordillera and occurring in the subsurface of adjacent Interior Plains. Major tectonostratigraphic assemblages are the latest Silurian-Eifelian platform carbonates and evaporites, the latest Eifelian-Frasnian basinal mudrocks with isolated carbonate banks bundled in the Horn River Group (HRG), and the thick coarsening-upward siliciclastic succession of Frasnian-Tournaisian age deposited in the distal setting of the Ellesmerian foreland basin. A major total petroleum system of the HRG defines the economic prospectivity of Devonian strata. Review of the lithostratigraphic nomenclature is supplemented with highlights on HRG depositional environments, patterns of thermal maturity, disconformities, and sedimentary cycles in platform carbonates.
GEOSCAN ID326094

 
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