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Cryogenic cave carbonates from the Cold Wind Cave, Nízke Tatry Mountains, Slovakia: Extending the age range of cryogenic cave carbonate formation to the Saalian
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SYSNO ASEP 0326034 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Cryogenic cave carbonates from the Cold Wind Cave, Nízke Tatry Mountains, Slovakia: Extending the age range of cryogenic cave carbonate formation to the Saalian Title Kryogenní jeskynní karbonáty z Jaskyně studeného vetra, Nízke Tatry, Slovensko: rozšíření období tvorby kryogenních jeskynních karbonátů do sálského glaciálu Author(s) Žák, Karel (GLU-S) SAI, RID, ORCID
Hercman, H. (PL)
Orvošová, M. (SK)
Jačková, I. (CZ)Source Title International Journal of Speleology. - : Societa Speleologica Italiana - ISSN 0392-6672
Roč. 38, č. 2 (2009), s. 139-152Number of pages 14 s. Publication form www - www Language eng - English Country IT - Italy Keywords cryogenic cave carbonate ; U-series dating ; carbon and oxygen stable isotopes ; Western Carpathians ; Nízké Tatry Mts. Subject RIV DB - Geology ; Mineralogy CEZ AV0Z30130516 - GLU-S (2005-2011) UT WOS 000268413400005 EID SCOPUS 67649845483 DOI 10.5038/1827-806X.38.2.5 Annotation Cold Wind Cave and Dead Bats Cave represent togehter a unique cave system with polyphase formation, located at high elevation in Nízke Tatry Mounains, Slovakia. The paper reviews evolution of the caves and describes cryogenic cave carbonates discovered in the Cold Wind Cave. Cryogenic cave carbonated were formed here during freezing of karst waters in Saalian and Weichselian glacils. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Year of Publishing 2009
Number of the records: 1