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TitleStable isotope and XRD data from the Lower-Middle Devonian carbonates with focus on paleosols, Northwest Territories, Canada
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Associated Datahttps://doi.org/10.1016/j.gloplacha.2021.103573
 
LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorKabanov, PORCID logo; Abdi, W; Bilot, I; Dwyer, W; Fontaine, R; Klassen, K; Middlestead, P; Percival, J BORCID logo; Pinard, J; Wygergangs, M
SourceGeological Survey of Canada, Open File 8815, 2021, 10 pages, https://doi.org/10.4095/328651 Open Access logo Open Access
Image
Year2021
PublisherNatural Resources Canada
Documentopen file
Lang.English
Mediaon-line; digital
File formatpdf
ProvinceNorthwest Territories
NTS95J/08; 95N/15; 107A/12
Lat/Long WENS-122.4031 -122.4028 62.3172 62.3169
Lat/Long WENS-124.6542 -124.6542 63.8833 63.8831
Lat/Long WENS-131.5244 -131.5244 68.5322 68.5319
Subjectsgeochemistry; mineralogy; sedimentology; Science and Technology; Nature and Environment; Middle Devonian; Lower Devonian; bedrock geology; lithology; sedimentary rocks; carbonates; paleosols; stable isotope studies; carbon isotopes; oxygen isotopes; x-ray diffraction analyses; exploration wells; core samples; sedimentary facies; bulk composition; size fractionation; clays; Landry Formation; Headless Formation; Kugaluk N-02 Well; Dahadinni 2M-43 Well; Ebbutt D-50 Well; Methodology; Phanerozoic; Paleozoic; Devonian
Illustrationstables
ProgramGEM-GeoNorth: Geo-mapping for Energy and Minerals GEM Program Coordination
Released2021 09 02
AbstractThis collection of data and description of lab protocols supplements publication (Kabanov, 2021). The diamond-drill cores from historical exploration wells of Northwest Territories, Canada, were sampled over the period from 2013 to 2020 for the study of subaerial exposure profiles (paleosols and paleokarsts) and other facies in the shallow-marine (peritidal) carbonates of the Early-Middle Devonian Landry and Headless formations. Samples were collected with hand tools under hand lens and, where required, binocular microscope. Stable carbon and oxygen measurements (delta-13C and delta-18O vs. VPDB) were performed at the Jan Veizer Stable Isotope Lab of the University of Ottawa. Mineralogy of 18 samples were completed by powder X-ray diffraction (XRD) analyses for bulk-rock and clay-size fractions at the Mineralogy Lab of GSC-Ottawa. Our analytical results provide the largest set of mineralogy and stable isotope data available from the Landry and Headless formations and can be reused in future projects exploring the diagenetic pathways of isotopic reset in these strata and the follow-up studies of subaerial exposure profiles. We also describe the curation procedure and give sample access information for the core and sample repository at GSC Calgary.
Summary(Plain Language Summary, not published)
This collection of data and description of lab protocols supplements publication (Kabanov, 2021). The diamond-drill cores from historical exploration wells of Northwest Territories, Canada, were sampled over the period from 2013 to 2020 for the study of subaerial exposure profiles (paleosols and paleokarsts) and other facies in the shallow-marine (peritidal) carbonates of the Lower-Middle Devonian Landry and Headless formations. Stable carbon and oxygen measurements (delta-13C and delta-18O vs. VPDB) were performed at the Jan Veizer Stable Isotope Lab of the University of Ottawa. Mineralogy of 18 samples were completed by powder X-ray diffraction (XRD) analyses for bulk-rock and clay-size fractions at the Mineralogy Lab of GSC-Ottawa. Our analytical results provide the largest set of mineralogy and stable isotope data available from the Landry and Headless formations and can be reused in future projects exploring the diagenetic pathways of isotopic reset in these strata and the follow-up studies of subaerial exposure profiles. We also describe the curation procedure and give sample access information for the core and sample repository at GSC Calgary.
GEOSCAN ID328651

 
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