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Statements

Subject Item
n2:RIV%2F67985831%3A_____%2F00%3A09013072%21RIV%2F2003%2FAV0%2FA09003%2FN
rdf:type
n17:Vysledek skos:Concept
dcterms:description
Vertical and subvertical pipes are circular to ovate in shape with diametres from 2-4 m up to tens of metres and with proven depth up to 82 m. Some of them terminate by horizontal cave levels at depth. Pipes are filled with complicated sedimentary sequences with clearly developed collapse structures. The fill is composed of pre-Cenomanian, Cenomanian-Turonian and Tertiary deposits. Internal structures of the fill indicate multiphase collapses. Cretaceous and pre-Cretaceous deposits are often subvertical with chaotic internal texture. In the centre of some of pipes, there are traces of younger collapses, most probably induced by continuing karstification and suffosion at depth. Tertiary deposits overlay the Cretaceous ones unconformably; they show gentler centripetal inclination, but in places they fill the central parts of collapsed fill. The origin of solution pipes is connected with hydrothermal activity most probably during Paleogene to Miocene, when the surface of limestones was still covered by s Vertical and subvertical pipes are circular to ovate in shape with diametres from 2-4 m up to tens of metres and with proven depth up to 82 m. Some of them terminate by horizontal cave levels at depth. Pipes are filled with complicated sedimentary sequences with clearly developed collapse structures. The fill is composed of pre-Cenomanian, Cenomanian-Turonian and Tertiary deposits. Internal structures of the fill indicate multiphase collapses. Cretaceous and pre-Cretaceous deposits are often subvertical with chaotic internal texture. In the centre of some of pipes, there are traces of younger collapses, most probably induced by continuing karstification and suffosion at depth. Tertiary deposits overlay the Cretaceous ones unconformably; they show gentler centripetal inclination, but in places they fill the central parts of collapsed fill. The origin of solution pipes is connected with hydrothermal activity most probably during Paleogene to Miocene, when the surface of limestones was still covered by s
dcterms:title
The evolution of karst and caves in the Koněprusy region (Bohemian Karst, Czech Republic), Part III: Collapse structures. The evolution of karst and caves in the Koněprusy region (Bohemian Karst, Czech Republic), Part III: Collapse structures.
skos:prefLabel
The evolution of karst and caves in the Koněprusy region (Bohemian Karst, Czech Republic), Part III: Collapse structures. The evolution of karst and caves in the Koněprusy region (Bohemian Karst, Czech Republic), Part III: Collapse structures.
skos:notation
RIV/67985831:_____/00:09013072!RIV/2003/AV0/A09003/N
n3:strany
35;50
n3:aktivita
n4:Z
n3:aktivity
Z(AV0Z3013912)
n3:dodaniDat
n5:2003
n3:domaciTvurceVysledku
n13:5788056
n3:druhVysledku
n18:C
n3:duvernostUdaju
n16:S
n3:entitaPredkladatele
n9:predkladatel
n3:idSjednocenehoVysledku
710705
n3:idVysledku
RIV/67985831:_____/00:09013072
n3:jazykVysledku
n14:eng
n3:klicovaSlova
paleokarst; hydrothermal karstification; collapse
n3:klicoveSlovo
n10:hydrothermal%20karstification n10:collapse n10:paleokarst
n3:kontrolniKodProRIV
[4B43A744AA3C]
n3:mistoVydani
Ljubljana
n3:nazevEdiceCisloSvazku
, 2
n3:nazevZdroje
Acta carsologica.
n3:obor
n6:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
1
n3:pocetUcastnikuAkce
0
n3:pocetZahranicnichUcastnikuAkce
0
n3:rokUplatneniVysledku
n5:2000
n3:tvurceVysledku
Bosák, Pavel
n3:zamer
n11:AV0Z3013912
s:numberOfPages
16
n7:hasPublisher
Slovenska Akademija znanosti in umetnosti