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The first isotopic data on the Paleoproterozoic age of the Serpovidnyi Ridge amphibolites, Keivy terrane, Baltic shield. / Myskova, T.A.; Balagansky, V.V.; Glebovitsky, V.A.; Lvov, P.A.; Mudruk, S.V.; Skublov, S.G.

In: Doklady Earth Sciences, No. 2, 2014, p. 1553-1558.

Research output: Contribution to journal › Article

Harvard

Myskova, TA, Balagansky, VV, Glebovitsky, VA, Lvov, PA, Mudruk, SV & Skublov, SG 2014, 'The first isotopic data on the Paleoproterozoic age of the Serpovidnyi Ridge amphibolites, Keivy terrane, Baltic shield', Doklady Earth Sciences, no. 2, pp. 1553-1558. https://doi.org/10.1134/S1028334X14120083

APA

Myskova, T. A., Balagansky, V. V., Glebovitsky, V. A., Lvov, P. A., Mudruk, S. V., & Skublov, S. G. (2014). The first isotopic data on the Paleoproterozoic age of the Serpovidnyi Ridge amphibolites, Keivy terrane, Baltic shield. Doklady Earth Sciences, (2), 1553-1558. https://doi.org/10.1134/S1028334X14120083

Vancouver

Myskova TA, Balagansky VV, Glebovitsky VA, Lvov PA, Mudruk SV, Skublov SG. The first isotopic data on the Paleoproterozoic age of the Serpovidnyi Ridge amphibolites, Keivy terrane, Baltic shield. Doklady Earth Sciences. 2014;(2):1553-1558. https://doi.org/10.1134/S1028334X14120083

Author

Myskova, T.A. ; Balagansky, V.V. ; Glebovitsky, V.A. ; Lvov, P.A. ; Mudruk, S.V. ; Skublov, S.G. / The first isotopic data on the Paleoproterozoic age of the Serpovidnyi Ridge amphibolites, Keivy terrane, Baltic shield. In: Doklady Earth Sciences. 2014 ; No. 2. pp. 1553-1558.

BibTeX

@article{787ebac02bf74282aa07cf0df80cb32b,
title = "The first isotopic data on the Paleoproterozoic age of the Serpovidnyi Ridge amphibolites, Keivy terrane, Baltic shield",
abstract = "{\textcopyright} 2014, Pleiades Publishing, Ltd. This work presents the first data on the geochemistry, U-Pb (SHRIMP-II) age of zircon, U-Pb (conventional) age of titanite, Sm-Nd model age of whole rock samples, and age of reworking of metaporphyric rocks of the Serpovidnyi Ridge of the Keivy structure. These rocks are characterized by high contents of trace and rare earth elements indicative of an origin of the rocks from the enriched mantle source EM2. The negative ɛNd value (−2.4) does not exclude the contamination of mantle material. The age of two close periods is reliably identified: the crystallization of zircon (1740 ± 15 Ma) and porphyroblastesis with the formation of plagioclase and epidote glomeroblasts combined with the crystallization of titanite (1719 ± 13 Ma). The Sm-Nd isotope data indicate the Paleoproterozoic age of mafic volcanism in the Keivy terrane (2.37–1.77 Ga).",
author = "T.A. Myskova and V.V. Balagansky and V.A. Glebovitsky and P.A. Lvov and S.V. Mudruk and S.G. Skublov",
year = "2014",
doi = "10.1134/S1028334X14120083",
language = "English",
pages = "1553--1558",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - The first isotopic data on the Paleoproterozoic age of the Serpovidnyi Ridge amphibolites, Keivy terrane, Baltic shield

AU - Myskova, T.A.

AU - Balagansky, V.V.

AU - Glebovitsky, V.A.

AU - Lvov, P.A.

AU - Mudruk, S.V.

AU - Skublov, S.G.

PY - 2014

Y1 - 2014

N2 - © 2014, Pleiades Publishing, Ltd. This work presents the first data on the geochemistry, U-Pb (SHRIMP-II) age of zircon, U-Pb (conventional) age of titanite, Sm-Nd model age of whole rock samples, and age of reworking of metaporphyric rocks of the Serpovidnyi Ridge of the Keivy structure. These rocks are characterized by high contents of trace and rare earth elements indicative of an origin of the rocks from the enriched mantle source EM2. The negative ɛNd value (−2.4) does not exclude the contamination of mantle material. The age of two close periods is reliably identified: the crystallization of zircon (1740 ± 15 Ma) and porphyroblastesis with the formation of plagioclase and epidote glomeroblasts combined with the crystallization of titanite (1719 ± 13 Ma). The Sm-Nd isotope data indicate the Paleoproterozoic age of mafic volcanism in the Keivy terrane (2.37–1.77 Ga).

AB - © 2014, Pleiades Publishing, Ltd. This work presents the first data on the geochemistry, U-Pb (SHRIMP-II) age of zircon, U-Pb (conventional) age of titanite, Sm-Nd model age of whole rock samples, and age of reworking of metaporphyric rocks of the Serpovidnyi Ridge of the Keivy structure. These rocks are characterized by high contents of trace and rare earth elements indicative of an origin of the rocks from the enriched mantle source EM2. The negative ɛNd value (−2.4) does not exclude the contamination of mantle material. The age of two close periods is reliably identified: the crystallization of zircon (1740 ± 15 Ma) and porphyroblastesis with the formation of plagioclase and epidote glomeroblasts combined with the crystallization of titanite (1719 ± 13 Ma). The Sm-Nd isotope data indicate the Paleoproterozoic age of mafic volcanism in the Keivy terrane (2.37–1.77 Ga).

U2 - 10.1134/S1028334X14120083

DO - 10.1134/S1028334X14120083

M3 - Article

SP - 1553

EP - 1558

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 7061319