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The Vendian age of granodiorites and plagiogranites of the Tallainskii complex (Baikal–Muya Belt) : U–Pb isotope data. / Rytsk, E. Yu; Salnikova, E. B.; Glebovitsky, V. A.; Velikoslavinsky, S. D.; Alekseev, I. A.; Fedoseenko, A. M.; Plotkina, Yu V.

In: Doklady Earth Sciences, Vol. 474, No. 1, 01.05.2017, p. 569-573.

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

Harvard

Rytsk, EY, Salnikova, EB, Glebovitsky, VA, Velikoslavinsky, SD, Alekseev, IA, Fedoseenko, AM & Plotkina, YV 2017, 'The Vendian age of granodiorites and plagiogranites of the Tallainskii complex (Baikal–Muya Belt): U–Pb isotope data', Doklady Earth Sciences, vol. 474, no. 1, pp. 569-573. https://doi.org/10.1134/S1028334X17050166

APA

Rytsk, E. Y., Salnikova, E. B., Glebovitsky, V. A., Velikoslavinsky, S. D., Alekseev, I. A., Fedoseenko, A. M., & Plotkina, Y. V. (2017). The Vendian age of granodiorites and plagiogranites of the Tallainskii complex (Baikal–Muya Belt): U–Pb isotope data. Doklady Earth Sciences, 474(1), 569-573. https://doi.org/10.1134/S1028334X17050166

Vancouver

Rytsk EY, Salnikova EB, Glebovitsky VA, Velikoslavinsky SD, Alekseev IA, Fedoseenko AM et al. The Vendian age of granodiorites and plagiogranites of the Tallainskii complex (Baikal–Muya Belt): U–Pb isotope data. Doklady Earth Sciences. 2017 May 1;474(1):569-573. https://doi.org/10.1134/S1028334X17050166

Author

Rytsk, E. Yu ; Salnikova, E. B. ; Glebovitsky, V. A. ; Velikoslavinsky, S. D. ; Alekseev, I. A. ; Fedoseenko, A. M. ; Plotkina, Yu V. / The Vendian age of granodiorites and plagiogranites of the Tallainskii complex (Baikal–Muya Belt) : U–Pb isotope data. In: Doklady Earth Sciences. 2017 ; Vol. 474, No. 1. pp. 569-573.

BibTeX

@article{fc9fa9cc40aa44efa9ef7e8271ce67b2,
title = "The Vendian age of granodiorites and plagiogranites of the Tallainskii complex (Baikal–Muya Belt): U–Pb isotope data",
abstract = "This work presents the results of U–Pb isotope dating of zircons from granodiorites and plagiogranites of the Tallainskii gabbro–granodiorite–plagiogranite complex of the Karalon–Mamakan zone of the Baikal–Muya belt, ascribed to the Tallainskii pluton. The age datings obtained for granodiorite of the Eleninskii massif (605 ± 6 Ma) and plagiogranite of the Ust-Berezovo massif (609 ± 6 Ma) are in close agreement within the limits of error. Taking into account previously published data, the emplacement of the Tallainskii complex occurred within the age interval of 615–603 Ma in connection with postcollision extension. The “island arc” geochemical characteristics of granodiorites and plagiogranites can be explained by magmatic differentiation and (or) participation in the formation of a melt source enriched in the suprasubduction component involved in petrogenesis during the preceding Neoproterozoic period.",
author = "Rytsk, {E. Yu} and Salnikova, {E. B.} and Glebovitsky, {V. A.} and Velikoslavinsky, {S. D.} and Alekseev, {I. A.} and Fedoseenko, {A. M.} and Plotkina, {Yu V.}",
year = "2017",
month = may,
day = "1",
doi = "10.1134/S1028334X17050166",
language = "English",
volume = "474",
pages = "569--573",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - The Vendian age of granodiorites and plagiogranites of the Tallainskii complex (Baikal–Muya Belt)

T2 - U–Pb isotope data

AU - Rytsk, E. Yu

AU - Salnikova, E. B.

AU - Glebovitsky, V. A.

AU - Velikoslavinsky, S. D.

AU - Alekseev, I. A.

AU - Fedoseenko, A. M.

AU - Plotkina, Yu V.

PY - 2017/5/1

Y1 - 2017/5/1

N2 - This work presents the results of U–Pb isotope dating of zircons from granodiorites and plagiogranites of the Tallainskii gabbro–granodiorite–plagiogranite complex of the Karalon–Mamakan zone of the Baikal–Muya belt, ascribed to the Tallainskii pluton. The age datings obtained for granodiorite of the Eleninskii massif (605 ± 6 Ma) and plagiogranite of the Ust-Berezovo massif (609 ± 6 Ma) are in close agreement within the limits of error. Taking into account previously published data, the emplacement of the Tallainskii complex occurred within the age interval of 615–603 Ma in connection with postcollision extension. The “island arc” geochemical characteristics of granodiorites and plagiogranites can be explained by magmatic differentiation and (or) participation in the formation of a melt source enriched in the suprasubduction component involved in petrogenesis during the preceding Neoproterozoic period.

AB - This work presents the results of U–Pb isotope dating of zircons from granodiorites and plagiogranites of the Tallainskii gabbro–granodiorite–plagiogranite complex of the Karalon–Mamakan zone of the Baikal–Muya belt, ascribed to the Tallainskii pluton. The age datings obtained for granodiorite of the Eleninskii massif (605 ± 6 Ma) and plagiogranite of the Ust-Berezovo massif (609 ± 6 Ma) are in close agreement within the limits of error. Taking into account previously published data, the emplacement of the Tallainskii complex occurred within the age interval of 615–603 Ma in connection with postcollision extension. The “island arc” geochemical characteristics of granodiorites and plagiogranites can be explained by magmatic differentiation and (or) participation in the formation of a melt source enriched in the suprasubduction component involved in petrogenesis during the preceding Neoproterozoic period.

UR - http://www.scopus.com/inward/record.url?scp=85020749058&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17050166

DO - 10.1134/S1028334X17050166

M3 - Article

AN - SCOPUS:85020749058

VL - 474

SP - 569

EP - 573

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 48490609