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The First Petrological Evidence for Subduction at the Western Margin of the Siberian Craton. / Likhanov, I. I.; Kozlov, P. S.; Savko, K. A. et al.

In: Doklady Earth Sciences, Vol. 484, No. 1, 01.07.2019, p. 79-83.

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

Harvard

Likhanov, II, Kozlov, PS, Savko, KA, Zinoviev, SV & Krylov, AA 2019, 'The First Petrological Evidence for Subduction at the Western Margin of the Siberian Craton', Doklady Earth Sciences, vol. 484, no. 1, pp. 79-83. https://doi.org/10.1134/S1028334X19010124

APA

Likhanov, I. I., Kozlov, P. S., Savko, K. A., Zinoviev, S. V., & Krylov, A. A. (2019). The First Petrological Evidence for Subduction at the Western Margin of the Siberian Craton. Doklady Earth Sciences, 484(1), 79-83. https://doi.org/10.1134/S1028334X19010124

Vancouver

Likhanov II, Kozlov PS, Savko KA, Zinoviev SV, Krylov AA. The First Petrological Evidence for Subduction at the Western Margin of the Siberian Craton. Doklady Earth Sciences. 2019 Jul 1;484(1):79-83. doi: 10.1134/S1028334X19010124

Author

Likhanov, I. I. ; Kozlov, P. S. ; Savko, K. A. et al. / The First Petrological Evidence for Subduction at the Western Margin of the Siberian Craton. In: Doklady Earth Sciences. 2019 ; Vol. 484, No. 1. pp. 79-83.

BibTeX

@article{58693d7458994ea8a3071d5bcd3362aa,
title = "The First Petrological Evidence for Subduction at the Western Margin of the Siberian Craton",
abstract = "Abstract: The discovery of relics of glaucophane schist in high-pressure tectonites of the suture zone of Yenisei Ridge has provided evidence for a Cordillera-type convergent boundary controlled by subduction of the oceanic crust beneath the continental margin on the western side of the Siberian Craton. According to the microtextural patterns of rocks and the results of geothermobarometry, two stages of metamorphism were distinguished. The formation of high-pressure tectonites indicates the early stage in the evolution of the Paleoasian Ocean and the final stage in the Neoproterozoic history of the Yenisei Ridge including completion of the accretion–subduction processes on the western margin of the Siberian Craton.",
keywords = "YENISEI RIDGE, EVOLUTION, EVENTS",
author = "Likhanov, {I. I.} and Kozlov, {P. S.} and Savko, {K. A.} and Zinoviev, {S. V.} and Krylov, {A. A.}",
year = "2019",
month = jul,
day = "1",
doi = "10.1134/S1028334X19010124",
language = "English",
volume = "484",
pages = "79--83",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - The First Petrological Evidence for Subduction at the Western Margin of the Siberian Craton

AU - Likhanov, I. I.

AU - Kozlov, P. S.

AU - Savko, K. A.

AU - Zinoviev, S. V.

AU - Krylov, A. A.

PY - 2019/7/1

Y1 - 2019/7/1

N2 - Abstract: The discovery of relics of glaucophane schist in high-pressure tectonites of the suture zone of Yenisei Ridge has provided evidence for a Cordillera-type convergent boundary controlled by subduction of the oceanic crust beneath the continental margin on the western side of the Siberian Craton. According to the microtextural patterns of rocks and the results of geothermobarometry, two stages of metamorphism were distinguished. The formation of high-pressure tectonites indicates the early stage in the evolution of the Paleoasian Ocean and the final stage in the Neoproterozoic history of the Yenisei Ridge including completion of the accretion–subduction processes on the western margin of the Siberian Craton.

AB - Abstract: The discovery of relics of glaucophane schist in high-pressure tectonites of the suture zone of Yenisei Ridge has provided evidence for a Cordillera-type convergent boundary controlled by subduction of the oceanic crust beneath the continental margin on the western side of the Siberian Craton. According to the microtextural patterns of rocks and the results of geothermobarometry, two stages of metamorphism were distinguished. The formation of high-pressure tectonites indicates the early stage in the evolution of the Paleoasian Ocean and the final stage in the Neoproterozoic history of the Yenisei Ridge including completion of the accretion–subduction processes on the western margin of the Siberian Craton.

KW - YENISEI RIDGE

KW - EVOLUTION

KW - EVENTS

UR - http://www.scopus.com/inward/record.url?scp=85064006489&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19010124

DO - 10.1134/S1028334X19010124

M3 - Article

AN - SCOPUS:85064006489

VL - 484

SP - 79

EP - 83

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 19359877