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From migmatites to crustal granites : Pb–Pb isotopic system of feldspars of partial melting products, Northern Ladoga region, Fennoscandinavian Shield. / Baltybaev, Sh K.; Ovchinnikova, G. V.; Glebovitskii, V. A.; Vasil’eva, I. M.; Rizvanova, N. G.

In: Doklady Earth Sciences, Vol. 468, No. 2, 01.06.2016, p. 541-544.

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

Harvard

Baltybaev, SK, Ovchinnikova, GV, Glebovitskii, VA, Vasil’eva, IM & Rizvanova, NG 2016, 'From migmatites to crustal granites: Pb–Pb isotopic system of feldspars of partial melting products, Northern Ladoga region, Fennoscandinavian Shield', Doklady Earth Sciences, vol. 468, no. 2, pp. 541-544. https://doi.org/10.1134/S1028334X16060015

APA

Baltybaev, S. K., Ovchinnikova, G. V., Glebovitskii, V. A., Vasil’eva, I. M., & Rizvanova, N. G. (2016). From migmatites to crustal granites: Pb–Pb isotopic system of feldspars of partial melting products, Northern Ladoga region, Fennoscandinavian Shield. Doklady Earth Sciences, 468(2), 541-544. https://doi.org/10.1134/S1028334X16060015

Vancouver

Baltybaev SK, Ovchinnikova GV, Glebovitskii VA, Vasil’eva IM, Rizvanova NG. From migmatites to crustal granites: Pb–Pb isotopic system of feldspars of partial melting products, Northern Ladoga region, Fennoscandinavian Shield. Doklady Earth Sciences. 2016 Jun 1;468(2):541-544. https://doi.org/10.1134/S1028334X16060015

Author

Baltybaev, Sh K. ; Ovchinnikova, G. V. ; Glebovitskii, V. A. ; Vasil’eva, I. M. ; Rizvanova, N. G. / From migmatites to crustal granites : Pb–Pb isotopic system of feldspars of partial melting products, Northern Ladoga region, Fennoscandinavian Shield. In: Doklady Earth Sciences. 2016 ; Vol. 468, No. 2. pp. 541-544.

BibTeX

@article{495ca6cc95804048a0cd1807f2f76cd4,
title = "From migmatites to crustal granites: Pb–Pb isotopic system of feldspars of partial melting products, Northern Ladoga region, Fennoscandinavian Shield",
abstract = "The isotopic–geochemical features of late and postorogenic granites of the S type and ambient migmatites are studied within the Russian part of the Svecofennian orogen of the Fennoscandinavian Shield. The spatial association of leucosomes of migmatites and granites of the S type and their similar petro- and geochemistry and distribution of Pb isotopes are evidence of the genetic similarity of their parental melts. The Borodinskoe pluton has a more primitive 206Pb/207Pb ratio, which indicates the presence of upper and U-poor lower crustal material in the source of granitic magmas. This conclusion is supported by the ɛNt(t) lower value of granites of this pluton relative to those of other plutons of the region.",
author = "Baltybaev, {Sh K.} and Ovchinnikova, {G. V.} and Glebovitskii, {V. A.} and Vasil{\textquoteright}eva, {I. M.} and Rizvanova, {N. G.}",
note = "Publisher Copyright: {\textcopyright} 2016, Pleiades Publishing, Ltd.",
year = "2016",
month = jun,
day = "1",
doi = "10.1134/S1028334X16060015",
language = "English",
volume = "468",
pages = "541--544",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - From migmatites to crustal granites

T2 - Pb–Pb isotopic system of feldspars of partial melting products, Northern Ladoga region, Fennoscandinavian Shield

AU - Baltybaev, Sh K.

AU - Ovchinnikova, G. V.

AU - Glebovitskii, V. A.

AU - Vasil’eva, I. M.

AU - Rizvanova, N. G.

N1 - Publisher Copyright: © 2016, Pleiades Publishing, Ltd.

PY - 2016/6/1

Y1 - 2016/6/1

N2 - The isotopic–geochemical features of late and postorogenic granites of the S type and ambient migmatites are studied within the Russian part of the Svecofennian orogen of the Fennoscandinavian Shield. The spatial association of leucosomes of migmatites and granites of the S type and their similar petro- and geochemistry and distribution of Pb isotopes are evidence of the genetic similarity of their parental melts. The Borodinskoe pluton has a more primitive 206Pb/207Pb ratio, which indicates the presence of upper and U-poor lower crustal material in the source of granitic magmas. This conclusion is supported by the ɛNt(t) lower value of granites of this pluton relative to those of other plutons of the region.

AB - The isotopic–geochemical features of late and postorogenic granites of the S type and ambient migmatites are studied within the Russian part of the Svecofennian orogen of the Fennoscandinavian Shield. The spatial association of leucosomes of migmatites and granites of the S type and their similar petro- and geochemistry and distribution of Pb isotopes are evidence of the genetic similarity of their parental melts. The Borodinskoe pluton has a more primitive 206Pb/207Pb ratio, which indicates the presence of upper and U-poor lower crustal material in the source of granitic magmas. This conclusion is supported by the ɛNt(t) lower value of granites of this pluton relative to those of other plutons of the region.

UR - http://www.scopus.com/inward/record.url?scp=84978541109&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16060015

DO - 10.1134/S1028334X16060015

M3 - Article

AN - SCOPUS:84978541109

VL - 468

SP - 541

EP - 544

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 93113673