In: Geologica Carpathica, vol. 60, no. 5
Milan Kohut - Pavel Uher - Marian Putis - Martin Ondrejka - Sergey Sergeev - Alexander Larionov - Ilya Paderin
Details:
Year, pages: 2009, 345 - 350
Language: eng
Keywords:
Western Carpathians, Male Karpaty Mts, Bratislava Massif, Modra Massif, granitic rocks, zircon, SHRIMP dating
Original source URL: http://www.geologicacarpathica.com/browse-journal/volumes/60-5/article-490/
About article:
Representative granitic rock samples from the Male Karpaty Mountains of the Western Carpathians (Slovakia) were dated by the SHRIMP U-Th-Pb isotope method on zircons. Oscillatory zoned zircons revealed concordant Mississippian magmatic ages: 355±5 Ma in Bratislava granodiorite, and 347±4 Ma in Modra tonalite. The results document nearly synchronous, successive Meso-Hercynian plutonic events from S-type to I-type granites. The Neo-Proterozoic inherited zircon cores (590±13 Ma) were identified in the Bratislava S-type granitic rocks whereas scarce Paleo-Proterozoic inherited zircons (1984±36 Ma) were detected within the Modra I-type tonalites.
How to cite:
ISO 690:
Kohut, M., Uher, P., Putis, M., Ondrejka, 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. In Geologica Carpathica, vol. 60, no.5, pp. 345-350. 1335-0552. DOI: https://doi.org/10.2478/v10096-009-0026-z
APA:
Kohut, M., Uher, P., Putis, M., Ondrejka, 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. 1335-0552. DOI: https://doi.org/10.2478/v10096-009-0026-z
About edition: