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Adakite-gabbro-anorthosite magmatism at the final (576–546 Ma) development stage of the Neoproterozoic active margin in the south-west of the Siberian craton. / Vernikovskaya, A. E.; Vernikovsky, V. A.; Matushkin, N. Yu et al.

In: Doklady Earth Sciences, Vol. 477, No. 2, 01.12.2017, p. 1402-1407.

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

Harvard

Vernikovskaya, AE, Vernikovsky, VA, Matushkin, NY, Kadilnikov, PI, Romanova, IV & Larionov, AN 2017, 'Adakite-gabbro-anorthosite magmatism at the final (576–546 Ma) development stage of the Neoproterozoic active margin in the south-west of the Siberian craton', Doklady Earth Sciences, vol. 477, no. 2, pp. 1402-1407. https://doi.org/10.1134/S1028334X17120108

APA

Vernikovskaya, A. E., Vernikovsky, V. A., Matushkin, N. Y., Kadilnikov, P. I., Romanova, I. V., & Larionov, A. N. (2017). Adakite-gabbro-anorthosite magmatism at the final (576–546 Ma) development stage of the Neoproterozoic active margin in the south-west of the Siberian craton. Doklady Earth Sciences, 477(2), 1402-1407. https://doi.org/10.1134/S1028334X17120108

Vancouver

Vernikovskaya AE, Vernikovsky VA, Matushkin NY, Kadilnikov PI, Romanova IV, Larionov AN. Adakite-gabbro-anorthosite magmatism at the final (576–546 Ma) development stage of the Neoproterozoic active margin in the south-west of the Siberian craton. Doklady Earth Sciences. 2017 Dec 1;477(2):1402-1407. doi: 10.1134/S1028334X17120108

Author

Vernikovskaya, A. E. ; Vernikovsky, V. A. ; Matushkin, N. Yu et al. / Adakite-gabbro-anorthosite magmatism at the final (576–546 Ma) development stage of the Neoproterozoic active margin in the south-west of the Siberian craton. In: Doklady Earth Sciences. 2017 ; Vol. 477, No. 2. pp. 1402-1407.

BibTeX

@article{35594bfd72474eda89bb3e4952a31c41,
title = "Adakite-gabbro-anorthosite magmatism at the final (576–546 Ma) development stage of the Neoproterozoic active margin in the south-west of the Siberian craton",
abstract = "In the late Neoproterozoic a prolonged active continental margin mode dominated the southwestern margin of the Siberian craton. Based on results of geological, petrological-geochemical, U–Th–Pb and Sm–Nd, Rb–Sr isotope investigations, for the first time we established that on the final evolution stage of this margin 576–546 Ma, intrusions of adakites and gabbro-anorthosites of the Zimoveyniy massif were emplaced in the South Yenisei Ridge. These new data indicate genetic relationships of the studied adakites and host NEB-metabasites. The formation of adakites could have been due to a crustal or a mantle-crustal source in a setting of transform sliding of lithospheric plates after the subduction stopped.",
author = "Vernikovskaya, {A. E.} and Vernikovsky, {V. A.} and Matushkin, {N. Yu} and Kadilnikov, {P. I.} and Romanova, {I. V.} and Larionov, {A. N.}",
year = "2017",
month = dec,
day = "1",
doi = "10.1134/S1028334X17120108",
language = "English",
volume = "477",
pages = "1402--1407",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Adakite-gabbro-anorthosite magmatism at the final (576–546 Ma) development stage of the Neoproterozoic active margin in the south-west of the Siberian craton

AU - Vernikovskaya, A. E.

AU - Vernikovsky, V. A.

AU - Matushkin, N. Yu

AU - Kadilnikov, P. I.

AU - Romanova, I. V.

AU - Larionov, A. N.

PY - 2017/12/1

Y1 - 2017/12/1

N2 - In the late Neoproterozoic a prolonged active continental margin mode dominated the southwestern margin of the Siberian craton. Based on results of geological, petrological-geochemical, U–Th–Pb and Sm–Nd, Rb–Sr isotope investigations, for the first time we established that on the final evolution stage of this margin 576–546 Ma, intrusions of adakites and gabbro-anorthosites of the Zimoveyniy massif were emplaced in the South Yenisei Ridge. These new data indicate genetic relationships of the studied adakites and host NEB-metabasites. The formation of adakites could have been due to a crustal or a mantle-crustal source in a setting of transform sliding of lithospheric plates after the subduction stopped.

AB - In the late Neoproterozoic a prolonged active continental margin mode dominated the southwestern margin of the Siberian craton. Based on results of geological, petrological-geochemical, U–Th–Pb and Sm–Nd, Rb–Sr isotope investigations, for the first time we established that on the final evolution stage of this margin 576–546 Ma, intrusions of adakites and gabbro-anorthosites of the Zimoveyniy massif were emplaced in the South Yenisei Ridge. These new data indicate genetic relationships of the studied adakites and host NEB-metabasites. The formation of adakites could have been due to a crustal or a mantle-crustal source in a setting of transform sliding of lithospheric plates after the subduction stopped.

UR - http://www.scopus.com/inward/record.url?scp=85039978055&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17120108

DO - 10.1134/S1028334X17120108

M3 - Article

AN - SCOPUS:85039978055

VL - 477

SP - 1402

EP - 1407

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 9409757