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Late Vendian postcollisional leucogranites of Yenisei Ridge. / Nozhkin, A. D.; Likhanov, I. I.; Reverdatto, V. V. et al.

In: Doklady Earth Sciences, Vol. 474, No. 2, 01.06.2017, p. 674-679.

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

Harvard

Nozhkin, AD, Likhanov, II, Reverdatto, VV, Bayanova, TB, Zinoviev, SV, Kozlov, PS, Popov, NV & Dmitrieva, NV 2017, 'Late Vendian postcollisional leucogranites of Yenisei Ridge', Doklady Earth Sciences, vol. 474, no. 2, pp. 674-679. https://doi.org/10.1134/S1028334X17060125

APA

Nozhkin, A. D., Likhanov, I. I., Reverdatto, V. V., Bayanova, T. B., Zinoviev, S. V., Kozlov, P. S., Popov, N. V., & Dmitrieva, N. V. (2017). Late Vendian postcollisional leucogranites of Yenisei Ridge. Doklady Earth Sciences, 474(2), 674-679. https://doi.org/10.1134/S1028334X17060125

Vancouver

Nozhkin AD, Likhanov II, Reverdatto VV, Bayanova TB, Zinoviev SV, Kozlov PS et al. Late Vendian postcollisional leucogranites of Yenisei Ridge. Doklady Earth Sciences. 2017 Jun 1;474(2):674-679. doi: 10.1134/S1028334X17060125

Author

Nozhkin, A. D. ; Likhanov, I. I. ; Reverdatto, V. V. et al. / Late Vendian postcollisional leucogranites of Yenisei Ridge. In: Doklady Earth Sciences. 2017 ; Vol. 474, No. 2. pp. 674-679.

BibTeX

@article{168bffe3b0f341db8a232834638dad1d,
title = "Late Vendian postcollisional leucogranites of Yenisei Ridge",
abstract = "The Late Vendian (540–550 Ma) U–Pb zircon age of postcollisional granitoids in the Osinovka Massif was obtained for the first time. The Osinovka Massif is located in rocks of the island-arc complex of the Isakovka Terrane, in the northwestern part of the Sayany–Yenisei accretion belt. These events stand for the final stage of the Neoproterozoic history of the Yenisei Ridge, related to the completing accretion of the oceanic crust fragments and the beginning of the Caledonian orogenesis. The petrogeochemical composition and the Sm–Nd isotopic characteristics support the fact that the granitoid melt originated from a highly differentiated continental crust of the southwestern margin of the Siberian Craton. Hence, the granite-bearing Late Riphean island-arc complexes were thrust over the craton margin at a distance considerably exceeding the dimensions of the Osinovka Massif.",
author = "Nozhkin, {A. D.} and Likhanov, {I. I.} and Reverdatto, {V. V.} and Bayanova, {T. B.} and Zinoviev, {S. V.} and Kozlov, {P. S.} and Popov, {N. V.} and Dmitrieva, {N. V.}",
year = "2017",
month = jun,
day = "1",
doi = "10.1134/S1028334X17060125",
language = "English",
volume = "474",
pages = "674--679",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Late Vendian postcollisional leucogranites of Yenisei Ridge

AU - Nozhkin, A. D.

AU - Likhanov, I. I.

AU - Reverdatto, V. V.

AU - Bayanova, T. B.

AU - Zinoviev, S. V.

AU - Kozlov, P. S.

AU - Popov, N. V.

AU - Dmitrieva, N. V.

PY - 2017/6/1

Y1 - 2017/6/1

N2 - The Late Vendian (540–550 Ma) U–Pb zircon age of postcollisional granitoids in the Osinovka Massif was obtained for the first time. The Osinovka Massif is located in rocks of the island-arc complex of the Isakovka Terrane, in the northwestern part of the Sayany–Yenisei accretion belt. These events stand for the final stage of the Neoproterozoic history of the Yenisei Ridge, related to the completing accretion of the oceanic crust fragments and the beginning of the Caledonian orogenesis. The petrogeochemical composition and the Sm–Nd isotopic characteristics support the fact that the granitoid melt originated from a highly differentiated continental crust of the southwestern margin of the Siberian Craton. Hence, the granite-bearing Late Riphean island-arc complexes were thrust over the craton margin at a distance considerably exceeding the dimensions of the Osinovka Massif.

AB - The Late Vendian (540–550 Ma) U–Pb zircon age of postcollisional granitoids in the Osinovka Massif was obtained for the first time. The Osinovka Massif is located in rocks of the island-arc complex of the Isakovka Terrane, in the northwestern part of the Sayany–Yenisei accretion belt. These events stand for the final stage of the Neoproterozoic history of the Yenisei Ridge, related to the completing accretion of the oceanic crust fragments and the beginning of the Caledonian orogenesis. The petrogeochemical composition and the Sm–Nd isotopic characteristics support the fact that the granitoid melt originated from a highly differentiated continental crust of the southwestern margin of the Siberian Craton. Hence, the granite-bearing Late Riphean island-arc complexes were thrust over the craton margin at a distance considerably exceeding the dimensions of the Osinovka Massif.

UR - http://www.scopus.com/inward/record.url?scp=85024129620&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17060125

DO - 10.1134/S1028334X17060125

M3 - Article

AN - SCOPUS:85024129620

VL - 474

SP - 674

EP - 679

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 12692269