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New data on the U-Pb (SHRIMP II) age of zircons from aluminous gneisses of the Archean Kola Group of the Baltic shield and the problem of their interpretation. / Myskova, T.A.; Mil’kevich, R.I.; Glebovitskii, V.A.; L’vov, P.A.; Berezhnaya, N.G.

In: Doklady Earth Sciences, No. 1, 2015, p. 738-745.

Research output: Contribution to journal › Article

Harvard

Myskova, TA, Mil’kevich, RI, Glebovitskii, VA, L’vov, PA & Berezhnaya, NG 2015, 'New data on the U-Pb (SHRIMP II) age of zircons from aluminous gneisses of the Archean Kola Group of the Baltic shield and the problem of their interpretation', Doklady Earth Sciences, no. 1, pp. 738-745. https://doi.org/10.1134/S1028334X15070211

APA

Myskova, T. A., Mil’kevich, R. I., Glebovitskii, V. A., L’vov, P. A., & Berezhnaya, N. G. (2015). New data on the U-Pb (SHRIMP II) age of zircons from aluminous gneisses of the Archean Kola Group of the Baltic shield and the problem of their interpretation. Doklady Earth Sciences, (1), 738-745. https://doi.org/10.1134/S1028334X15070211

Vancouver

Myskova TA, Mil’kevich RI, Glebovitskii VA, L’vov PA, Berezhnaya NG. New data on the U-Pb (SHRIMP II) age of zircons from aluminous gneisses of the Archean Kola Group of the Baltic shield and the problem of their interpretation. Doklady Earth Sciences. 2015;(1):738-745. https://doi.org/10.1134/S1028334X15070211

Author

Myskova, T.A. ; Mil’kevich, R.I. ; Glebovitskii, V.A. ; L’vov, P.A. ; Berezhnaya, N.G. / New data on the U-Pb (SHRIMP II) age of zircons from aluminous gneisses of the Archean Kola Group of the Baltic shield and the problem of their interpretation. In: Doklady Earth Sciences. 2015 ; No. 1. pp. 738-745.

BibTeX

@article{e116f9d9bfb844d39daa35d044478ac4,
title = "New data on the U-Pb (SHRIMP II) age of zircons from aluminous gneisses of the Archean Kola Group of the Baltic shield and the problem of their interpretation",
abstract = "{\textcopyright} 2015, Pleiades Publishing, Ltd.New data on the U-Pb (SHRIMP II) age are obtained for aluminous gneisses of the Kola Group of the Baltic shield. Gneisses are typically ascribed to metasedimentary rocks with detrital zircons. Our work interprets the isotopic data based on the magmatic (tonalite) origin of gneisses and zircon that was established from study of the morphology and geochemistry of zircons. The age of crystallization of the protolith is 2.9 Ga. The existence of two stages of Archean granulite metamorphism is confirmed: an early stage (2.9 Ga) and later granulite metamorphism (2707–2656 Ma).",
author = "T.A. Myskova and R.I. Mil{\textquoteright}kevich and V.A. Glebovitskii and P.A. L{\textquoteright}vov and N.G. Berezhnaya",
year = "2015",
doi = "10.1134/S1028334X15070211",
language = "English",
pages = "738--745",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - New data on the U-Pb (SHRIMP II) age of zircons from aluminous gneisses of the Archean Kola Group of the Baltic shield and the problem of their interpretation

AU - Myskova, T.A.

AU - Mil’kevich, R.I.

AU - Glebovitskii, V.A.

AU - L’vov, P.A.

AU - Berezhnaya, N.G.

PY - 2015

Y1 - 2015

N2 - © 2015, Pleiades Publishing, Ltd.New data on the U-Pb (SHRIMP II) age are obtained for aluminous gneisses of the Kola Group of the Baltic shield. Gneisses are typically ascribed to metasedimentary rocks with detrital zircons. Our work interprets the isotopic data based on the magmatic (tonalite) origin of gneisses and zircon that was established from study of the morphology and geochemistry of zircons. The age of crystallization of the protolith is 2.9 Ga. The existence of two stages of Archean granulite metamorphism is confirmed: an early stage (2.9 Ga) and later granulite metamorphism (2707–2656 Ma).

AB - © 2015, Pleiades Publishing, Ltd.New data on the U-Pb (SHRIMP II) age are obtained for aluminous gneisses of the Kola Group of the Baltic shield. Gneisses are typically ascribed to metasedimentary rocks with detrital zircons. Our work interprets the isotopic data based on the magmatic (tonalite) origin of gneisses and zircon that was established from study of the morphology and geochemistry of zircons. The age of crystallization of the protolith is 2.9 Ga. The existence of two stages of Archean granulite metamorphism is confirmed: an early stage (2.9 Ga) and later granulite metamorphism (2707–2656 Ma).

U2 - 10.1134/S1028334X15070211

DO - 10.1134/S1028334X15070211

M3 - Article

SP - 738

EP - 745

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 4001784