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Carboniferous Granitoid Magmatism of Northern Taimyr : Results of Isotopic-Geochemical Study and Geodynamic Interpretation. / Kurapov, M. Yu. ; Ershova, V. B. ; Makariev, A. A. ; Makarieva, E. V. ; Khudoley, A. K. ; Luchitskaya, M. V. ; Prokopiev, A. V. .

In: Geotectonics, Vol. 52, No. 2, 01.03.2018, p. 225-239.

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

Harvard

Kurapov, MY, Ershova, VB, Makariev, AA, Makarieva, EV, Khudoley, AK, Luchitskaya, MV & Prokopiev, AV 2018, 'Carboniferous Granitoid Magmatism of Northern Taimyr: Results of Isotopic-Geochemical Study and Geodynamic Interpretation', Geotectonics, vol. 52, no. 2, pp. 225-239. https://doi.org/10.1134/S0016852118020048

APA

Kurapov, M. Y., Ershova, V. B., Makariev, A. A., Makarieva, E. V., Khudoley, A. K., Luchitskaya, M. V., & Prokopiev, A. V. (2018). Carboniferous Granitoid Magmatism of Northern Taimyr: Results of Isotopic-Geochemical Study and Geodynamic Interpretation. Geotectonics, 52(2), 225-239. https://doi.org/10.1134/S0016852118020048

Vancouver

Kurapov MY, Ershova VB, Makariev AA, Makarieva EV, Khudoley AK, Luchitskaya MV et al. Carboniferous Granitoid Magmatism of Northern Taimyr: Results of Isotopic-Geochemical Study and Geodynamic Interpretation. Geotectonics. 2018 Mar 1;52(2):225-239. https://doi.org/10.1134/S0016852118020048

Author

Kurapov, M. Yu. ; Ershova, V. B. ; Makariev, A. A. ; Makarieva, E. V. ; Khudoley, A. K. ; Luchitskaya, M. V. ; Prokopiev, A. V. . / Carboniferous Granitoid Magmatism of Northern Taimyr : Results of Isotopic-Geochemical Study and Geodynamic Interpretation. In: Geotectonics. 2018 ; Vol. 52, No. 2. pp. 225-239.

BibTeX

@article{856b753472574814af752f38a76fc4c5,
title = "Carboniferous Granitoid Magmatism of Northern Taimyr: Results of Isotopic-Geochemical Study and Geodynamic Interpretation",
abstract = "Data on the petrography, geochemistry, and isotopic geochronology of granites from the northern part of the Taimyr Peninsula are considered. The Early–Middle Carboniferous age of these rocks has been established (U–Pb, SIMS). Judging by the results of 40Ar/ 39Ar dating, the rocks underwent metamorphism in the Middle Permian. In geochemical and isotopic composition, the granitic rocks have much in common with evolved I-type granites. This makes it possible to specify a suprasubduction marginal continental formation setting. The existence of an active Carboniferous margin along the southern edge of the Kara Block (in presentday coordinates) corroborates the close relationship of the studied region with the continent of Baltia. ",
keywords = "I-type granite, Permian metamorphism, Taimyr, active margin, syncollisional granites",
author = "Kurapov, {M. Yu.} and Ershova, {V. B.} and Makariev, {A. A.} and Makarieva, {E. V.} and Khudoley, {A. K.} and Luchitskaya, {M. V.} and Prokopiev, {A. V.}",
year = "2018",
month = mar,
day = "1",
doi = "10.1134/S0016852118020048",
language = "English",
volume = "52",
pages = "225--239",
journal = "Geotectonics",
issn = "0016-8521",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Carboniferous Granitoid Magmatism of Northern Taimyr

T2 - Results of Isotopic-Geochemical Study and Geodynamic Interpretation

AU - Kurapov, M. Yu.

AU - Ershova, V. B.

AU - Makariev, A. A.

AU - Makarieva, E. V.

AU - Khudoley, A. K.

AU - Luchitskaya, M. V.

AU - Prokopiev, A. V.

PY - 2018/3/1

Y1 - 2018/3/1

N2 - Data on the petrography, geochemistry, and isotopic geochronology of granites from the northern part of the Taimyr Peninsula are considered. The Early–Middle Carboniferous age of these rocks has been established (U–Pb, SIMS). Judging by the results of 40Ar/ 39Ar dating, the rocks underwent metamorphism in the Middle Permian. In geochemical and isotopic composition, the granitic rocks have much in common with evolved I-type granites. This makes it possible to specify a suprasubduction marginal continental formation setting. The existence of an active Carboniferous margin along the southern edge of the Kara Block (in presentday coordinates) corroborates the close relationship of the studied region with the continent of Baltia.

AB - Data on the petrography, geochemistry, and isotopic geochronology of granites from the northern part of the Taimyr Peninsula are considered. The Early–Middle Carboniferous age of these rocks has been established (U–Pb, SIMS). Judging by the results of 40Ar/ 39Ar dating, the rocks underwent metamorphism in the Middle Permian. In geochemical and isotopic composition, the granitic rocks have much in common with evolved I-type granites. This makes it possible to specify a suprasubduction marginal continental formation setting. The existence of an active Carboniferous margin along the southern edge of the Kara Block (in presentday coordinates) corroborates the close relationship of the studied region with the continent of Baltia.

KW - I-type granite

KW - Permian metamorphism

KW - Taimyr

KW - active margin

KW - syncollisional granites

UR - http://www.scopus.com/inward/record.url?scp=85045615950&partnerID=8YFLogxK

U2 - 10.1134/S0016852118020048

DO - 10.1134/S0016852118020048

M3 - Article

VL - 52

SP - 225

EP - 239

JO - Geotectonics

JF - Geotectonics

SN - 0016-8521

IS - 2

ER -

ID: 35198899