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Magnetic fabric and mineralogy of cave deposits in Botovskaya Cave (Eastern Siberia, Russian Federation)
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SYSNO ASEP 0394978 Document Type C - Proceedings Paper (int. conf.) R&D Document Type Conference Paper Title Magnetic fabric and mineralogy of cave deposits in Botovskaya Cave (Eastern Siberia, Russian Federation) Author(s) Kadlec, Jaroslav (GLU-S) RID, SAI, ORCID
Hercman, H. (PL)
Chadima, Martin (GLU-S) RID, SAI
Lisá, Lenka (GLU-S) RID, SAI, ORCID
Oberhänsli, H. (DE)
Osintsev, A. (RU)Source Title 16th International Congress of Speleology : Czech Republic, Brno July 21-28, 2013 : proceedings, 3. - Prague : Česká speleologická společnost, 2013 / Filippi M. ; Bosák P. - ISBN 978-80-87857-09-0 Pages s. 96-98 Number of pages 3 s. Publication form Print - P Action International Congress of Speleology /16./ Event date 21.07.2013-28.07.2013 VEvent location Brno Country CZ - Czech Republic Event type WRD Language eng - English Country CZ - Czech Republic Keywords caves ; magnetic fabric ; mineralogy ; cave deposits Subject RIV DB - Geology ; Mineralogy Institutional support GLU-S - RVO:67985831 CEZ AV0Z30130516 - GLU-S (2005-2011) Annotation The Botovskaya Cave is a typical example of a two-dimensional maze with a total length of explored passages exceeding 60 km, which represents the longest limestone cave system in the Russian Federation. The clastic cave sediments filling the cave passages differ in both mineral and mineral magnetic properties and were deposited under different hydrological conditions. The older portion of the clastic cave fills was derived from overlying sandstones, whereas the properties of younger cave sediments show closer affinity to the soils and weathering products originating on the sandstone plateau above the cave. The cave sediments underwent repeated periods of deposition and erosion during the Tertiary and Pleistocene. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Year of Publishing 2014
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