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TitleLithostratigraphy of Devonian basinal mudrocks in frontier areas of northwestern Canada augmented with ED-XRF technique
 
AuthorKabanov, PORCID logo; Vandenberg, RORCID logo; Pelchat, P; Cameron, M; Dewing, KORCID logo
Sourcearktos 2020 p. 1-14, https://doi.org/10.1007/s41063-020-00074-z
Image
Year2020
Alt SeriesNatural Resources Canada, Contribution Series 20180326
PublisherSpinger
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
ProvinceNorthwest Territories; Nunavut
NTS87C; 87E; 87F; 87G; 87H; 88; 89A; 89B; 96C; 96D; 96E; 96F; 96G; 96J; 96K; 96L; 96M; 96N; 96O; 96P; 97; 98; 99A; 106; 107; 116A; 116H; 116I; 116P; 117A; 117D
AreaMackenzie River; Mackenzie Delta; Norman Wells; Beaufort Sea; Arctic Ocean; Canadian Arctic Islands; Banks Island; Melville Island; Prince Patrick Island
Lat/Long WENS-137.0000 -108.0000 76.5000 64.0000
Subjectsregional geology; stratigraphy; geochemistry; Science and Technology; Nature and Environment; bedrock geology; lithology; sedimentary rocks; shales; siltstones; sandstones; limestones; cherts; dolostones; exploration wells; core samples; x-ray fluorescence analyses; lithostratigraphy; stratigraphic correlations; boreholes; trace element analyses; major element analyses; sedimentary wedges; sulphur geochemistry; iron geochemistry; manganese geochemistry; aluminum geochemistry; molybdenum geochemistry; oxides; isotopic studies; carbon isotopes; Kugaluk N-02 Well; Orksut I-44 Well; Nanuk D-76 Well; Little Bear N-09 Well; Loon Creek O-06 Well; Devonian Anoxic Events; Ancestral North America; Laurentia; Mackenzie-Peel Platform; Norman Wells Oil Field; Horn River Group; Tuttle Formation; Imperial Formation; Blackley Member; Weatherall Formation; Hecla Formation; Canol Formation; Kee Scarp; Mirror Lake Member; Dodo Canyon Member; Vermillion Creek Member; Hare Indian Formation; Bell Creek Member; Prohibition Creek Member; Francis Creek Member; Bluefish Member; Orksut Formation; Kitson Formation; Cape de Bray Formation; Blackley Formation; Hume Formation; Headless Member; Landry Formation; Blue Fiord Formation; Anderson Plain; Mackenzie King Group; Christopher Formation; Phanerozoic; Paleozoic; Devonian
Illustrationslocation maps; geoscientific sketch maps; photographs; stratigraphic charts; correlation charts; tables; lithologic sections; profiles; correlation sections
ProgramGEM: Geo-mapping for Energy and Minerals Sverdrup Sedimentary Basin
Released2020 03 04
AbstractRock materials from three Arctic wells drilled through Middle-Upper Devonian basinal mudrocks between 1969 and 1973 were surveyed with the energy-dispersive X-ray fluorescence tool (ED-XRF) Bruker Tracer IV-SD(TM). The logs of major oxides acquired from cuttings of two wells on Banks Island show that lithological signals can be seen through sample contamination, and therefore are capable of significantly increasing litho-chemostratigraphic resolution of old borehole logs. Survey of major and trace elements on a cored section through visually monotonous black shales of the Kugaluk N-02 well in northern mainland N.W.T. reveals new details, which allows for the correlation of this reference section with a better-studied succession in the central Northwest Territories, as well as the interpretation of anoxic horizons which correlate globally as the 'Devonian anoxic events'. Despite shortcomings in accuracy, ED-XRF proves to be a rapid non-destructive technique to gain new information from old exploration wells in remote frontier areas.
Summary(Plain Language Summary, not published)
Rock materials from three Arctic wells drilled through Middle-Upper Devonian basinal mudrocks in 1969-1973 were surveyed with the energy-dispersive X-ray fluorescence tool (ED-XRF) Brooker Tracer IV-SD. The logs of major oxides acquired from cuttings of two wells on Banks Island show that lithological signals manifest through sample contamination, hence are capable to significantly increase litho-chemostratigraphic resolution of old borehole logs. Survey of major and trace elements on a cored section through visually monotonous black shales of Kugaluk N-02 well in northern mainland N.W.T. reveals many new details, which allows to correlate this reference section with better-studied succession in the central N.W.T. and interpret anoxic horizons that may correlate globally with the Devonian 'black-shale events'. Despite shortcomings in accuracy, ED-XRF proves to be an excellent non-destructive technique to gain new information from old exploration wells in remote frontier areas.
GEOSCAN ID313311

 
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