Title | Geological and geochemical data from Mackenzie corridor. Part XI: New geochemical, magnetic susceptibility, and X-ray diffraction data from the Horn River Group (Devonian) in cores and outcrops south of
Norman Wells, Northwest Territories |
Download | Downloads |
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Licence | Please note the adoption of the Open Government Licence - Canada
supersedes any previous licences. |
Author | Kabanov, P B ;
Abdi, W; Biggin, A J ; Bilot, I; van der Boon, A ; Gouwy, S ; Grasby, S ; Minions, N; Percival, J ; Thallner, D; Twemlow, C; VandenBerg, R |
Source | Geological Survey of Canada, Open File 8940, 2023, 13 pages, https://doi.org/10.4095/331201 Open Access |
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Year | 2023 |
Publisher | Natural Resources Canada |
Document | open file |
Lang. | English |
Media | digital; on-line |
Related | NRCan photo(s) in this
publication |
File format | readme
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File format | pdf; docx; jpg; xlsx |
Province | Northwest Territories |
NTS | 96E/01; 96E/02 |
Area | Norman Wells; Prohibition Creek; Loon Creek; Mirror Lake; Little Bear |
Lat/Long WENS | -127.0000 -126.0000 65.2500 65.0000 |
Subjects | geochemistry; general geology; mineralogy; x-ray diffraction; nitrogen; carbon isotopes; data collections; core analysis; core samples; isotopic studies; Horn River Group; Mackenzie Corridor |
Illustrations | cross-sections; photographs; location maps; ternary diagrams; graphs |
Program | GEM2: Geo-mapping for Energy and Minerals GEM Synthesis |
Released | 2023 01 12 |
Summary | (Plain Language Summary, not published) This report compiles previously unpublished analytical data from two cores and an outcrop section of the sedimentary rocks of Middle-Upper Devonian age
bundled in the Horn River Group in central Mackenzie Valley between Norman Wells and Tulita. This includes a broad range of high-precision elemental geochemical data, carbon and oxygen stable isotope data, mineral composition based on X-ray
diffraction data, pyrolysis data providing parameters of fossil organic matter, and magnetic siusceptibility measurements. These data are used in two recent publications. Scientific implications of this study shed light on redox systems in Devonian
black-shale basins globally, including signatures and nature of multiple anoxic events, the conditions that were conductive for vigorous stocking and preservation of planktogenic organic matter in many shelfal basins of the world. This line of
research aslo explores the greenhouse (warm and ice-free) state of Earth surface in the remote Past and therefore has relevance to predict the ultimate state of the global warming. |
GEOSCAN ID | 331201 |
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