Standard
SHRIMP U-Th-Pb zircon dating of the granitoid massifs in the Male Karpaty Mountains (Western Carpathians): evidence of Meso-Hercynian successive S- to I-type granitic magmatism. / Kohut, M.; Uher, P.; Putis, M.; Ondreika, M.; Sergeev, S.; Larionov, A.; Paderin, I.
в:
Geologica Carpathica, Том 60, № 5, 2009, стр. 345-350.
Результаты исследований: Научные публикации в периодических изданиях › статья
Harvard
Kohut, M, Uher, P, Putis, M, Ondreika, M
, Sergeev, S, Larionov, A & Paderin, I 2009, '
SHRIMP U-Th-Pb zircon dating of the granitoid massifs in the Male Karpaty Mountains (Western Carpathians): evidence of Meso-Hercynian successive S- to I-type granitic magmatism.',
Geologica Carpathica, Том. 60, № 5, стр. 345-350.
APA
Kohut, M., Uher, P., Putis, M., Ondreika, M.
, Sergeev, S., Larionov, A., & Paderin, I. (2009).
SHRIMP U-Th-Pb zircon dating of the granitoid massifs in the Male Karpaty Mountains (Western Carpathians): evidence of Meso-Hercynian successive S- to I-type granitic magmatism. Geologica Carpathica,
60(5), 345-350.
Vancouver
Author
BibTeX
@article{86b1262462024fd38a8a6b12b2938856,
title = "SHRIMP U-Th-Pb zircon dating of the granitoid massifs in the Male Karpaty Mountains (Western Carpathians): evidence of Meso-Hercynian successive S- to I-type granitic magmatism.",
author = "M. Kohut and P. Uher and M. Putis and M. Ondreika and S. Sergeev and A. Larionov and I. Paderin",
year = "2009",
language = "не определен",
volume = "60",
pages = "345--350",
journal = "Geologica Carpathica",
issn = "1335-0552",
publisher = "Slovak Academic Press Ltd",
number = "5",
}
RIS
TY - JOUR
T1 - SHRIMP U-Th-Pb zircon dating of the granitoid massifs in the Male Karpaty Mountains (Western Carpathians): evidence of Meso-Hercynian successive S- to I-type granitic magmatism.
AU - Kohut, M.
AU - Uher, P.
AU - Putis, M.
AU - Ondreika, M.
AU - Sergeev, S.
AU - Larionov, A.
AU - Paderin, I.
PY - 2009
Y1 - 2009
M3 - статья
VL - 60
SP - 345
EP - 350
JO - Geologica Carpathica
JF - Geologica Carpathica
SN - 1335-0552
IS - 5
ER -