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Tracing metamorphism, exhumation and topographic evolution in orogenic belts by multiple thermochronology: a case study from the Nízke Tatry Mts., Western Carpathians
- 1.0365627 - GLÚ 2012 RIV CH eng J - Journal Article
Danišík, M. - Kadlec, Jaroslav - Glotzbach, Ch. - Weisheit, A. - Dunkl, I. - Kohút, M. - Evans, N. J. - Orvošová, M. - McDonald, B. J.
Tracing metamorphism, exhumation and topographic evolution in orogenic belts by multiple thermochronology: a case study from the Nízke Tatry Mts., Western Carpathians.
Swiss Journal of Geosciences. Roč. 104, č. 2 (2011), s. 285-298. ISSN 1661-8726. E-ISSN 1661-8734
R&D Projects: GA AV ČR IAA3013201
Institutional research plan: CEZ:AV0Z30130516
Keywords : (U–Th–[Sm])/He dating * fission track dating * thermal modelling * exhumation * zircon * apatite * Nízké Tatry Mts. * Western Carpathians
Subject RIV: DB - Geology ; Mineralogy
Impact factor: 0.879, year: 2011
Anotace v originále: A combination of four thermochronometers [zircon fission track (ZFT), zircon (U–Th)/He (ZHe), apatite fission track (AFT) and apatite (U–Th–[Sm])/He (AHe) dating methods] applied to a valley to ridge transect is used to resolve the issues of metamorphic, exhumation and topographic evolution of the Nízke Tatry Mts. The ZFT ages revealed a rapid Eocene cooling event. Early Miocene AHe ages and thermal modelling results suggest that the samples were heated to temperatures of ~55–90_C during Oligocene– Miocene times.
Permanent Link: http://hdl.handle.net/11104/0200822
Number of the records: 1