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TitleResults of the U-Pb age of detrital zircons from Upper Proterozoic deposits of the eastern slope of the Anabar Uplift
 
AuthorKuptsova, A V; Khudoley, A K; Davis, WORCID logo; Ranbird, R H; Molchanov, A V
SourceStratigraphy and Geological Correlation vol. 23, issue 3, 2015 p. 246-261, https://doi.org/10.1134/S0869593815030053
Image
Year2015
Alt SeriesNatural Resources Canada, Contribution Series 20180108
PublisherPleiades Publishing Ltd
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
AreaBiringinde River; Malaya Kuonamka River; Myunyusyakh River; Russian Federation
Lat/Long WENS 113.5000 114.5000 69.2500 69.0000
Subjectsregional geology; stratigraphy; geochronology; radiometric dating; uranium lead dating; zircon dates; lead lead dates; uranium thorium ratios; provenance; terrigenous deposits; stratigraphic correlations; wells; bedrock geology; lithology; melange; sedimentary rocks; carbonates; conglomerates; sandstones; siltstones; claystones; dolomites; arkoses; igneous rocks; volcanic rocks; tuffs; lavas; intrusive rocks; intrusions; dykes; sedimentary structures; brecciation; petrographic analyses; morphology; Archean; Anabar Shield; Anabar Uplift; East Anabar Basin; Taimyr Orogen; Mukun Group; Billyakh Group; Kotuikan Formation; Yusmastakh Formation; Starorechenskaya Formation; Precambrian; Proterozoic
Illustrationslocation maps; geoscientific sketch maps; correlation sections; photomicrographs; tables; histograms; plots; Concordia diagrams
ProgramGEM: Geo-mapping for Energy and Minerals PGE/Base Metals - Victoria Island (NWT and Nunavut)
Released2015 06 05
AbstractThe Upper Proterozoic sequence in the southern part of the East Anabar Basin, as throughout the entire framing of the Anabar uplift, has a two-unit terrigenous-carbonate structure. The results of the U-Pb dating of detrital zircons show that there is a difference in stratigraphy of Riphean strata in the north and south of the Anabar Uplift. In the north, deposits of the entire sequence are regarded as Early Riphean; in the south, the thickness of these deposits is reduced to 70 m. The overlying stratum is regarded as Upper Riphean-Vendian. As the strata in the southern part of the East Anabar Basin strata are of younger (Late Riphean-Vendian) age, they cannot be assigned to the Mukun and Billyakh groups. The Riphean-Vendian deposits accumulated mainly through erosion of crystalline rocks of the Anabar Uplift. In the upper part of the sequence, the Vendian magmatic complexes located probably within the Taimyr Orogen played a significant role as provenance areas.
GEOSCAN ID308338

 
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