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The Vendian Vorogovka Group of Yenisei Ridge : Chemostratigraphy and results of U–Pb dating of detrital zircons. / Vishnevskaya, I. A.; Letnikova, E. F.; Proshenkin, A. I. et al.

In: Doklady Earth Sciences, Vol. 476, No. 1, 01.09.2017, p. 1016-1020.

Research output: Contribution to journal › Article › peer-review

Harvard

Vishnevskaya, IA, Letnikova, EF, Proshenkin, AI, Maslov, AV, Blagovidov, VV, Metelkin, DV & Priyatkina, NS 2017, 'The Vendian Vorogovka Group of Yenisei Ridge: Chemostratigraphy and results of U–Pb dating of detrital zircons', Doklady Earth Sciences, vol. 476, no. 1, pp. 1016-1020. https://doi.org/10.1134/S1028334X17090306

APA

Vishnevskaya, I. A., Letnikova, E. F., Proshenkin, A. I., Maslov, A. V., Blagovidov, V. V., Metelkin, D. V., & Priyatkina, N. S. (2017). The Vendian Vorogovka Group of Yenisei Ridge: Chemostratigraphy and results of U–Pb dating of detrital zircons. Doklady Earth Sciences, 476(1), 1016-1020. https://doi.org/10.1134/S1028334X17090306

Vancouver

Vishnevskaya IA, Letnikova EF, Proshenkin AI, Maslov AV, Blagovidov VV, Metelkin DV et al. The Vendian Vorogovka Group of Yenisei Ridge: Chemostratigraphy and results of U–Pb dating of detrital zircons. Doklady Earth Sciences. 2017 Sept 1;476(1):1016-1020. doi: 10.1134/S1028334X17090306

Author

Vishnevskaya, I. A. ; Letnikova, E. F. ; Proshenkin, A. I. et al. / The Vendian Vorogovka Group of Yenisei Ridge : Chemostratigraphy and results of U–Pb dating of detrital zircons. In: Doklady Earth Sciences. 2017 ; Vol. 476, No. 1. pp. 1016-1020.

BibTeX

@article{600b8e27e86b4f79be9b48e63061ef83,
title = "The Vendian Vorogovka Group of Yenisei Ridge: Chemostratigraphy and results of U–Pb dating of detrital zircons",
abstract = "Application of the method of isotope stratigraphy showed that the 87Sr/86Sr ratio in the least altered carbonate rocks of the Severnaya Rechka and Sukhaya Rechka formations in the Vorogovka Group of Yenisei Ridge ranges from 0.70813 to 0.70828, and δ13C varies from –0.7 to +1.8‰. Comparison of these data with similar data for the Late Precambrian sequences from other regions provides evidence for the Vendian age of the Vorogovka Group. This is supported by the results of LA ICP-MS U–Pb dating of detrital zircons from sandstone of the Severnaya Rechka Formation, which is the basal level of the group: the mid-weight age of the youngest zircon population is 584 ± 3 Ma.",
keywords = "EVOLUTION",
author = "Vishnevskaya, {I. A.} and Letnikova, {E. F.} and Proshenkin, {A. I.} and Maslov, {A. V.} and Blagovidov, {V. V.} and Metelkin, {D. V.} and Priyatkina, {N. S.}",
note = "Publisher Copyright: {\textcopyright} 2017, Pleiades Publishing, Ltd.",
year = "2017",
month = sep,
day = "1",
doi = "10.1134/S1028334X17090306",
language = "English",
volume = "476",
pages = "1016--1020",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - The Vendian Vorogovka Group of Yenisei Ridge

T2 - Chemostratigraphy and results of U–Pb dating of detrital zircons

AU - Vishnevskaya, I. A.

AU - Letnikova, E. F.

AU - Proshenkin, A. I.

AU - Maslov, A. V.

AU - Blagovidov, V. V.

AU - Metelkin, D. V.

AU - Priyatkina, N. S.

N1 - Publisher Copyright: © 2017, Pleiades Publishing, Ltd.

PY - 2017/9/1

Y1 - 2017/9/1

N2 - Application of the method of isotope stratigraphy showed that the 87Sr/86Sr ratio in the least altered carbonate rocks of the Severnaya Rechka and Sukhaya Rechka formations in the Vorogovka Group of Yenisei Ridge ranges from 0.70813 to 0.70828, and δ13C varies from –0.7 to +1.8‰. Comparison of these data with similar data for the Late Precambrian sequences from other regions provides evidence for the Vendian age of the Vorogovka Group. This is supported by the results of LA ICP-MS U–Pb dating of detrital zircons from sandstone of the Severnaya Rechka Formation, which is the basal level of the group: the mid-weight age of the youngest zircon population is 584 ± 3 Ma.

AB - Application of the method of isotope stratigraphy showed that the 87Sr/86Sr ratio in the least altered carbonate rocks of the Severnaya Rechka and Sukhaya Rechka formations in the Vorogovka Group of Yenisei Ridge ranges from 0.70813 to 0.70828, and δ13C varies from –0.7 to +1.8‰. Comparison of these data with similar data for the Late Precambrian sequences from other regions provides evidence for the Vendian age of the Vorogovka Group. This is supported by the results of LA ICP-MS U–Pb dating of detrital zircons from sandstone of the Severnaya Rechka Formation, which is the basal level of the group: the mid-weight age of the youngest zircon population is 584 ± 3 Ma.

KW - EVOLUTION

UR - http://www.scopus.com/inward/record.url?scp=85030719577&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17090306

DO - 10.1134/S1028334X17090306

M3 - Article

AN - SCOPUS:85030719577

VL - 476

SP - 1016

EP - 1020

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 9030361