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The Proterozoic Pogor’uy Formation of Yenisei Ridge : Age and Provenance Sources According to U/Pb Dating of Detrital Zircons. / Priyatkina, N. S.; Kuznetsov, N. B.; Rud’ko, S. V.; Shatsillo, A. V.; Khudoley, A. K.; Romanyuk, T. V.; Maslov, A. V.

In: Doklady Earth Sciences, Vol. 484, No. 1, 01.07.2019, p. 28-31.

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

Harvard

Priyatkina, NS, Kuznetsov, NB, Rud’ko, SV, Shatsillo, AV, Khudoley, AK, Romanyuk, TV & Maslov, AV 2019, 'The Proterozoic Pogor’uy Formation of Yenisei Ridge: Age and Provenance Sources According to U/Pb Dating of Detrital Zircons', Doklady Earth Sciences, vol. 484, no. 1, pp. 28-31. https://doi.org/10.1134/S1028334X19010136

APA

Priyatkina, N. S., Kuznetsov, N. B., Rud’ko, S. V., Shatsillo, A. V., Khudoley, A. K., Romanyuk, T. V., & Maslov, A. V. (2019). The Proterozoic Pogor’uy Formation of Yenisei Ridge: Age and Provenance Sources According to U/Pb Dating of Detrital Zircons. Doklady Earth Sciences, 484(1), 28-31. https://doi.org/10.1134/S1028334X19010136

Vancouver

Priyatkina NS, Kuznetsov NB, Rud’ko SV, Shatsillo AV, Khudoley AK, Romanyuk TV et al. The Proterozoic Pogor’uy Formation of Yenisei Ridge: Age and Provenance Sources According to U/Pb Dating of Detrital Zircons. Doklady Earth Sciences. 2019 Jul 1;484(1):28-31. https://doi.org/10.1134/S1028334X19010136

Author

Priyatkina, N. S. ; Kuznetsov, N. B. ; Rud’ko, S. V. ; Shatsillo, A. V. ; Khudoley, A. K. ; Romanyuk, T. V. ; Maslov, A. V. / The Proterozoic Pogor’uy Formation of Yenisei Ridge : Age and Provenance Sources According to U/Pb Dating of Detrital Zircons. In: Doklady Earth Sciences. 2019 ; Vol. 484, No. 1. pp. 28-31.

BibTeX

@article{69fe9c025e5842f5bbccd4bd9d545160,
title = "The Proterozoic Pogor{\textquoteright}uy Formation of Yenisei Ridge: Age and Provenance Sources According to U/Pb Dating of Detrital Zircons",
abstract = "The results of U-Pb-isotopic dating of detrital zircons from sandstones of the Proterozoic Pogor'uy Formation, occurring to the north and south of the East Angara block of Yenisei Ridge, are presented. The sandstones of the northern part of the East Angara block are dominated by Archean and Paleoproterozoic populations of detrital zircons, while the samples from the southern part of the East Angara block have been revealed up to 25% of Mesoproterozoic age grains. The detrital zircon ages allow limiting the maximum sedimentary age of the Pogor'uy Fm. and the entire interval of its formation to 1.2-0.9 Ga. The paleogeographic features of the Pogor'uy Fm. deposition in the context of the existing opinions on the location of Siberia within the Rodinia supercontinent were examined.",
keywords = "GEOCHRONOLOGY, MARGIN",
author = "Priyatkina, {N. S.} and Kuznetsov, {N. B.} and Rud{\textquoteright}ko, {S. V.} and Shatsillo, {A. V.} and Khudoley, {A. K.} and Romanyuk, {T. V.} and Maslov, {A. V.}",
year = "2019",
month = jul,
day = "1",
doi = "10.1134/S1028334X19010136",
language = "English",
volume = "484",
pages = "28--31",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - The Proterozoic Pogor’uy Formation of Yenisei Ridge

T2 - Age and Provenance Sources According to U/Pb Dating of Detrital Zircons

AU - Priyatkina, N. S.

AU - Kuznetsov, N. B.

AU - Rud’ko, S. V.

AU - Shatsillo, A. V.

AU - Khudoley, A. K.

AU - Romanyuk, T. V.

AU - Maslov, A. V.

PY - 2019/7/1

Y1 - 2019/7/1

N2 - The results of U-Pb-isotopic dating of detrital zircons from sandstones of the Proterozoic Pogor'uy Formation, occurring to the north and south of the East Angara block of Yenisei Ridge, are presented. The sandstones of the northern part of the East Angara block are dominated by Archean and Paleoproterozoic populations of detrital zircons, while the samples from the southern part of the East Angara block have been revealed up to 25% of Mesoproterozoic age grains. The detrital zircon ages allow limiting the maximum sedimentary age of the Pogor'uy Fm. and the entire interval of its formation to 1.2-0.9 Ga. The paleogeographic features of the Pogor'uy Fm. deposition in the context of the existing opinions on the location of Siberia within the Rodinia supercontinent were examined.

AB - The results of U-Pb-isotopic dating of detrital zircons from sandstones of the Proterozoic Pogor'uy Formation, occurring to the north and south of the East Angara block of Yenisei Ridge, are presented. The sandstones of the northern part of the East Angara block are dominated by Archean and Paleoproterozoic populations of detrital zircons, while the samples from the southern part of the East Angara block have been revealed up to 25% of Mesoproterozoic age grains. The detrital zircon ages allow limiting the maximum sedimentary age of the Pogor'uy Fm. and the entire interval of its formation to 1.2-0.9 Ga. The paleogeographic features of the Pogor'uy Fm. deposition in the context of the existing opinions on the location of Siberia within the Rodinia supercontinent were examined.

KW - GEOCHRONOLOGY

KW - MARGIN

UR - http://www.scopus.com/inward/record.url?scp=85063981138&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19010136

DO - 10.1134/S1028334X19010136

M3 - Article

AN - SCOPUS:85063981138

VL - 484

SP - 28

EP - 31

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 42210829