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Kuznechensky massif of K-rich porphyric granites : U-Pb data and tectonic position (Baltic shield). / Baltybaev, Sh K.; Sal'nikova, E. B.; Glebovitskij, V. A.; Berezhnaya, N. G.; Yakovleva, S. Z.; Kovach, V. P.

в: Doklady Akademii Nauk, Том 398, № 4, 2004, стр. 519-523.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Baltybaev, SK, Sal'nikova, EB, Glebovitskij, VA, Berezhnaya, NG, Yakovleva, SZ & Kovach, VP 2004, 'Kuznechensky massif of K-rich porphyric granites: U-Pb data and tectonic position (Baltic shield)', Doklady Akademii Nauk, Том. 398, № 4, стр. 519-523.

APA

Baltybaev, S. K., Sal'nikova, E. B., Glebovitskij, V. A., Berezhnaya, N. G., Yakovleva, S. Z., & Kovach, V. P. (2004). Kuznechensky massif of K-rich porphyric granites: U-Pb data and tectonic position (Baltic shield). Doklady Akademii Nauk, 398(4), 519-523.

Vancouver

Baltybaev SK, Sal'nikova EB, Glebovitskij VA, Berezhnaya NG, Yakovleva SZ, Kovach VP. Kuznechensky massif of K-rich porphyric granites: U-Pb data and tectonic position (Baltic shield). Doklady Akademii Nauk. 2004;398(4):519-523.

Author

Baltybaev, Sh K. ; Sal'nikova, E. B. ; Glebovitskij, V. A. ; Berezhnaya, N. G. ; Yakovleva, S. Z. ; Kovach, V. P. / Kuznechensky massif of K-rich porphyric granites : U-Pb data and tectonic position (Baltic shield). в: Doklady Akademii Nauk. 2004 ; Том 398, № 4. стр. 519-523.

BibTeX

@article{1ef5758216834e348865c354d33441ec,
title = "Kuznechensky massif of K-rich porphyric granites: U-Pb data and tectonic position (Baltic shield)",
abstract = "It is shown that the Svekofennian time of continent-arc collision is accompanied by at least two periods of high-silica porphyric K-rich granites formation, which are separated by several tens of millions years. The presented U-Pb-dating results for zircon and monazite from Kuznechensky intrusion granites confirm the intrusion formation on the orogenic stage.",
author = "Baltybaev, {Sh K.} and Sal'nikova, {E. B.} and Glebovitskij, {V. A.} and Berezhnaya, {N. G.} and Yakovleva, {S. Z.} and Kovach, {V. P.}",
year = "2004",
language = "English",
volume = "398",
pages = "519--523",
journal = "ДОКЛАДЫ АКАДЕМИИ НАУК",
issn = "0869-5652",
publisher = "Издательство {"}Наука{"}",
number = "4",

}

RIS

TY - JOUR

T1 - Kuznechensky massif of K-rich porphyric granites

T2 - U-Pb data and tectonic position (Baltic shield)

AU - Baltybaev, Sh K.

AU - Sal'nikova, E. B.

AU - Glebovitskij, V. A.

AU - Berezhnaya, N. G.

AU - Yakovleva, S. Z.

AU - Kovach, V. P.

PY - 2004

Y1 - 2004

N2 - It is shown that the Svekofennian time of continent-arc collision is accompanied by at least two periods of high-silica porphyric K-rich granites formation, which are separated by several tens of millions years. The presented U-Pb-dating results for zircon and monazite from Kuznechensky intrusion granites confirm the intrusion formation on the orogenic stage.

AB - It is shown that the Svekofennian time of continent-arc collision is accompanied by at least two periods of high-silica porphyric K-rich granites formation, which are separated by several tens of millions years. The presented U-Pb-dating results for zircon and monazite from Kuznechensky intrusion granites confirm the intrusion formation on the orogenic stage.

UR - http://www.scopus.com/inward/record.url?scp=12244296186&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:12244296186

VL - 398

SP - 519

EP - 523

JO - ДОКЛАДЫ АКАДЕМИИ НАУК

JF - ДОКЛАДЫ АКАДЕМИИ НАУК

SN - 0869-5652

IS - 4

ER -

ID: 93115762