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Cave sediments from the Postojnska-Planinska cave system (Slovenia): evidence of multi-phase evolution in epiphreatic zone
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SYSNO ASEP 0312825 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Cave sediments from the Postojnska-Planinska cave system (Slovenia): evidence of multi-phase evolution in epiphreatic zone Title Jeskynní sedimenty systému Postojnska-Planinska jama (Slovinsko): příklad vícefázového vývoje v epifreatické zóně Author(s) Zupan Hajna, N. (SI)
Pruner, Petr (GLU-S) RID, SAI, ORCID
Mihevc, A. (SI)
Schnabl, Petr (GLU-S) RID, SAI, ORCID
Bosák, Pavel (GLU-S) RID, SAISource Title Acta carsologica. - : Inštitut za raziskovanje krasa - ISSN 0583-6050
Roč. 37, č. 1 (2008), s. 63-86Number of pages 24 s. Publication form WWW - WWW Language eng - English Country SI - Slovenia Keywords dating ; palaeomagnetism ; magnetostratigraphy ; karst geomorphology ; Classical Karst Subject RIV DB - Geology ; Mineralogy R&D Projects IAA300130701 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) CEZ AV0Z30130516 - GLU-S (2005-2011) UT WOS 000259475300006 EID SCOPUS 52949135895 DOI https://doi.org/10.3986/ac.v37i1.160 Annotation The Postojnska jama–Planinska jama cave system and number of smaller caves between them are developed in the Postojnski kras situated between two dextral strike-slip fault zones of the Dinaric direction. Homogeneity of palaeomagnetic data can indicate fast deposition during short-lasted single-flood events. Such depositional style was favourable for record of short-lived excursions of the palaeomagnetic field. Most of studied sediments are younger than 0.78 Ma, some dates can indicate age deeply below 0.78 Ma. The cave system shows long evolution governed by the function of the Planinsko polje in the relation to the evolution of resurgence area in Ljubljana Moor farther on the east. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Tel.: 226 800 273 Year of Publishing 2009
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