Standard
Early Migmatites in the Prograde Metamorphism Zone of Gneisses in the Northern Domain of the Ladoga Region: U-Pb Evidence Based on Monazite. / Baltybaev, Sh.K.; Levchenkov, O.A.; Glebovitsky, V.A.; Kuz’mina, E.V.; Rizvanova, N.G.; Makeev, A.F.; Levsky, L.K.
в:
ДОКЛАДЫ АКАДЕМИИ НАУК, Том 420, № 4, 2008, стр. 504-506.
Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Harvard
Baltybaev, SK, Levchenkov, OA
, Glebovitsky, VA, Kuz’mina, EV, Rizvanova, NG, Makeev, AF & Levsky, LK 2008, '
Early Migmatites in the Prograde Metamorphism Zone of Gneisses in the Northern Domain of the Ladoga Region: U-Pb Evidence Based on Monazite.',
ДОКЛАДЫ АКАДЕМИИ НАУК, Том. 420, № 4, стр. 504-506.
APA
Baltybaev, S. K., Levchenkov, O. A.
, Glebovitsky, V. A., Kuz’mina, E. V., Rizvanova, N. G., Makeev, A. F., & Levsky, L. K. (2008).
Early Migmatites in the Prograde Metamorphism Zone of Gneisses in the Northern Domain of the Ladoga Region: U-Pb Evidence Based on Monazite. ДОКЛАДЫ АКАДЕМИИ НАУК,
420(4), 504-506.
Vancouver
Author
BibTeX
@article{a582d073961643aa831dbb6096020a43,
title = "Early Migmatites in the Prograde Metamorphism Zone of Gneisses in the Northern Domain of the Ladoga Region: U-Pb Evidence Based on Monazite.",
author = "Sh.K. Baltybaev and O.A. Levchenkov and V.A. Glebovitsky and E.V. Kuz{\textquoteright}mina and N.G. Rizvanova and A.F. Makeev and L.K. Levsky",
year = "2008",
language = "не определен",
volume = "420",
pages = "504--506",
journal = "ДОКЛАДЫ АКАДЕМИИ НАУК",
issn = "0869-5652",
publisher = "Издательство {"}Наука{"}",
number = "4",
}
RIS
TY - JOUR
T1 - Early Migmatites in the Prograde Metamorphism Zone of Gneisses in the Northern Domain of the Ladoga Region: U-Pb Evidence Based on Monazite.
AU - Baltybaev, Sh.K.
AU - Levchenkov, O.A.
AU - Glebovitsky, V.A.
AU - Kuz’mina, E.V.
AU - Rizvanova, N.G.
AU - Makeev, A.F.
AU - Levsky, L.K.
PY - 2008
Y1 - 2008
M3 - статья
VL - 420
SP - 504
EP - 506
JO - ДОКЛАДЫ АКАДЕМИИ НАУК
JF - ДОКЛАДЫ АКАДЕМИИ НАУК
SN - 0869-5652
IS - 4
ER -
