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A different duration of the formation of leucosome of migmatites in the K- and Na-zones of the northern Ladoga region of the southeastern Svecofennian belt, Fennoscandian shield. / Baltybaev, Sh K.; Glebovistkii, V. A.; Rizvanova, N. G.; Fedoseenko, A. M.; Lobikov, A. F.

In: Doklady Earth Sciences, Vol. 459, No. 1, 06.12.2014, p. 1333-1337.

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

Harvard

Baltybaev, SK, Glebovistkii, VA, Rizvanova, NG, Fedoseenko, AM & Lobikov, AF 2014, 'A different duration of the formation of leucosome of migmatites in the K- and Na-zones of the northern Ladoga region of the southeastern Svecofennian belt, Fennoscandian shield', Doklady Earth Sciences, vol. 459, no. 1, pp. 1333-1337. https://doi.org/10.1134/S1028334X1410002X

APA

Baltybaev, S. K., Glebovistkii, V. A., Rizvanova, N. G., Fedoseenko, A. M., & Lobikov, A. F. (2014). A different duration of the formation of leucosome of migmatites in the K- and Na-zones of the northern Ladoga region of the southeastern Svecofennian belt, Fennoscandian shield. Doklady Earth Sciences, 459(1), 1333-1337. https://doi.org/10.1134/S1028334X1410002X

Vancouver

Baltybaev SK, Glebovistkii VA, Rizvanova NG, Fedoseenko AM, Lobikov AF. A different duration of the formation of leucosome of migmatites in the K- and Na-zones of the northern Ladoga region of the southeastern Svecofennian belt, Fennoscandian shield. Doklady Earth Sciences. 2014 Dec 6;459(1):1333-1337. https://doi.org/10.1134/S1028334X1410002X

Author

Baltybaev, Sh K. ; Glebovistkii, V. A. ; Rizvanova, N. G. ; Fedoseenko, A. M. ; Lobikov, A. F. / A different duration of the formation of leucosome of migmatites in the K- and Na-zones of the northern Ladoga region of the southeastern Svecofennian belt, Fennoscandian shield. In: Doklady Earth Sciences. 2014 ; Vol. 459, No. 1. pp. 1333-1337.

BibTeX

@article{d14dfd9da9694f04bac13362e02a115e,
title = "A different duration of the formation of leucosome of migmatites in the K- and Na-zones of the northern Ladoga region of the southeastern Svecofennian belt, Fennoscandian shield",
abstract = "The duration of migmatite formation in the K and Na geochemical zones was first estimated for the Svecofennides of the northern Ladoga region. The U-Pb (TIMS) age of monazite was determined for the most complete sequence of leucosomes with geological control of their relations and relative age observed in the outcrops. The duration of formation of the leucosomes in two zones is different and is not overlapped by the error of the age analysis: about 5 and no less than 10–15 Ma in the K and Na zones, respectively. The different duration of migmatite formation may reflect different temperature evolution of the rocks of the two zones and also the influence of the composition and rheological properties of migmatizing sequences, which govern the conditions of liquation, transportation, and crystallization of the anatectic melt.",
author = "Baltybaev, {Sh K.} and Glebovistkii, {V. A.} and Rizvanova, {N. G.} and Fedoseenko, {A. M.} and Lobikov, {A. F.}",
note = "Publisher Copyright: {\textcopyright} 2014, Pleiades Publishing, Ltd.",
year = "2014",
month = dec,
day = "6",
doi = "10.1134/S1028334X1410002X",
language = "English",
volume = "459",
pages = "1333--1337",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - A different duration of the formation of leucosome of migmatites in the K- and Na-zones of the northern Ladoga region of the southeastern Svecofennian belt, Fennoscandian shield

AU - Baltybaev, Sh K.

AU - Glebovistkii, V. A.

AU - Rizvanova, N. G.

AU - Fedoseenko, A. M.

AU - Lobikov, A. F.

N1 - Publisher Copyright: © 2014, Pleiades Publishing, Ltd.

PY - 2014/12/6

Y1 - 2014/12/6

N2 - The duration of migmatite formation in the K and Na geochemical zones was first estimated for the Svecofennides of the northern Ladoga region. The U-Pb (TIMS) age of monazite was determined for the most complete sequence of leucosomes with geological control of their relations and relative age observed in the outcrops. The duration of formation of the leucosomes in two zones is different and is not overlapped by the error of the age analysis: about 5 and no less than 10–15 Ma in the K and Na zones, respectively. The different duration of migmatite formation may reflect different temperature evolution of the rocks of the two zones and also the influence of the composition and rheological properties of migmatizing sequences, which govern the conditions of liquation, transportation, and crystallization of the anatectic melt.

AB - The duration of migmatite formation in the K and Na geochemical zones was first estimated for the Svecofennides of the northern Ladoga region. The U-Pb (TIMS) age of monazite was determined for the most complete sequence of leucosomes with geological control of their relations and relative age observed in the outcrops. The duration of formation of the leucosomes in two zones is different and is not overlapped by the error of the age analysis: about 5 and no less than 10–15 Ma in the K and Na zones, respectively. The different duration of migmatite formation may reflect different temperature evolution of the rocks of the two zones and also the influence of the composition and rheological properties of migmatizing sequences, which govern the conditions of liquation, transportation, and crystallization of the anatectic melt.

UR - http://www.scopus.com/inward/record.url?scp=84914696740&partnerID=8YFLogxK

U2 - 10.1134/S1028334X1410002X

DO - 10.1134/S1028334X1410002X

M3 - Article

AN - SCOPUS:84914696740

VL - 459

SP - 1333

EP - 1337

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 93114027