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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
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SYSNO ASEP 0365627 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Tracing metamorphism, exhumation and topographic evolution in orogenic belts by multiple thermochronology: a case study from the Nízke Tatry Mts., Western Carpathians Author(s) Danišík, M. (AU)
Kadlec, Jaroslav (GLU-S) RID, SAI, ORCID
Glotzbach, Ch. (DE)
Weisheit, A. (DE)
Dunkl, I. (DE)
Kohút, M. (SK)
Evans, N. J. (AU)
Orvošová, M. (SK)
McDonald, B. J. (AU)Source Title Swiss Journal of Geosciences - ISSN 1661-8726
Roč. 104, č. 2 (2011), s. 285-298Number of pages 14 s. Publication form WWW - WWW Language eng - English Country CH - Switzerland Keywords (U–Th–[Sm])/He dating ; fission track dating ; thermal modelling ; exhumation ; zircon ; apatite ; Nízké Tatry Mts. ; Western Carpathians Subject RIV DB - Geology ; Mineralogy R&D Projects IAA3013201 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) CEZ AV0Z30130516 - GLU-S (2005-2011) UT WOS 000296377600006 EID SCOPUS 80955180994 DOI 10.1007/s00015-011-0060-6 Annotation 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. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Year of Publishing 2012
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