About: Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation)

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About: Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation) Goto Sponge NotDistinct Permalink

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	Klastické sedimenty v Botovské jeskyni se ukládaly ve dvou obdobích, jak bylo zjištěno pomocí magneto-mineralogických a mineralogických metod. Zdrojem starších sedimentů jsou pískovce, tvořící podloží i nadloží zkrasovělých vápenců. Zdrojem mladších sedimentů jsou pedogenezí postižené produkty zvětrávání, přemístěné do podzemí z povrchu nad jeskynním systémem. (cs) 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 plateau above the cave. The cave sediments underwent repeated periods of deposition and erosion during the Tertiary (?) and Pleistocene. The last catastrophic erosion event occurred in the cave more than 350 ka based on flowstone dating. Water seeping through the overlying sandstone body causes collapses of sandstone slabs from the cave passage ceilings, forming the youngest portion of the clastic cave fills. 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 plateau above the cave. The cave sediments underwent repeated periods of deposition and erosion during the Tertiary (?) and Pleistocene. The last catastrophic erosion event occurred in the cave more than 350 ka based on flowstone dating. Water seeping through the overlying sandstone body causes collapses of sandstone slabs from the cave passage ceilings, forming the youngest portion of the clastic cave fills. (en)
Title	Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation) Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation) (en) Klastické jeskynní sedimenty v Botovské jeskyni (Východní Sibiř, Rusko) (cs)
skos:prefLabel	Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation) Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation) (en) Klastické jeskynní sedimenty v Botovské jeskyni (Východní Sibiř, Rusko) (cs)
skos:notation	RIV/67985831:_____/08:00322272!RIV09-AV0-67985831
http://linked.open...avai/riv/aktivita	Z
http://linked.open...avai/riv/aktivity	Z(AV0Z30130516)
http://linked.open...iv/cisloPeriodika	3
http://linked.open...vai/riv/dodaniDat	2009
http://linked.open...aciTvurceVysledku	Lisá, Lenka Chadima, Martin Kadlec, Jaroslav
http://linked.open.../riv/druhVysledku	J - Článek v odborném periodiku
http://linked.open...iv/duvernostUdaju	S - Úplné a pravdivé údaje nepodléhající ochraně podle zvláštních právních předpisů
http://linked.open...titaPredkladatele	Geologický ústav AV ČR, v. v. i.
http://linked.open...dnocenehoVysledku	360110
http://linked.open...ai/riv/idVysledku	RIV/67985831:_____/08:00322272
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	cave sediments; mineral magnetism; Botovskaya Cave (en)
http://linked.open.../riv/klicoveSlovo	cave sediments Botovskaya Cave mineral magnetism
http://linked.open...odStatuVydavatele	US - Spojené státy americké
http://linked.open...ontrolniKodProRIV	[EED064FF1DE5]
http://linked.open...i/riv/nazevZdroje	Journal of Cave and Karst Studies
http://linked.open...in/vavai/riv/obor	DE
http://linked.open...ichTvurcuVysledku	3 (xsd:int)
http://linked.open...cetTvurcuVysledku	6 (xsd:int)
http://linked.open...UplatneniVysledku	2008
http://linked.open...v/svazekPeriodika	70
http://linked.open...iv/tvurceVysledku	Kadlec, Jaroslav Lisá, Lenka Chadima, Martin Hercman, H. Oberhänsli, H. Osintsev, A.
http://linked.open...ain/vavai/riv/wos	000263275600002
http://linked.open...n/vavai/riv/zamer	Zemský systém v průsečíku geologických procesů, vývoje života, klimatických a antropogenních vlivů
issn	1090-6924
number of pages	14 (xsd:int)
is http://linked.open...avai/riv/vysledek of	Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation) Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation) Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation) Clastic cave deposits in Botovskaya cave (Eastern Siberia, Russian Federation)

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