About: Baiyun Cave the longest cave in the Naigu shilin. – in South China Karst     Goto   Sponge   NotDistinct   Permalink

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  • The formation of the Baiyun Cave is directly connected with the development of the Naigu shilin. The formation of the karst underground and surface features depends on the regional tectonic deformation on the Cenozoic extension of the studied area. Younger, dramatic lowering of the ground-water level probably caused faster development of the shilin. Modern formation of the shilin at the surface is, beside other factors, influenced by the intensive dissolution of those lowered parts that are covered by soil and vegetation thus generating greater quantities of CO2 and more intensive dissolution of the rock which results in over-saturated water in the cave.
  • The formation of the Baiyun Cave is directly connected with the development of the Naigu shilin. The formation of the karst underground and surface features depends on the regional tectonic deformation on the Cenozoic extension of the studied area. Younger, dramatic lowering of the ground-water level probably caused faster development of the shilin. Modern formation of the shilin at the surface is, beside other factors, influenced by the intensive dissolution of those lowered parts that are covered by soil and vegetation thus generating greater quantities of CO2 and more intensive dissolution of the rock which results in over-saturated water in the cave. (en)
Title
  • Baiyun Cave the longest cave in the Naigu shilin. – in South China Karst
  • Baiyun Cave the longest cave in the Naigu shilin. – in South China Karst (en)
skos:prefLabel
  • Baiyun Cave the longest cave in the Naigu shilin. – in South China Karst
  • Baiyun Cave the longest cave in the Naigu shilin. – in South China Karst (en)
skos:notation
  • RIV/67985831:_____/11:00361401!RIV12-AV0-67985831
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(AV0Z30130516)
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 187760
http://linked.open...ai/riv/idVysledku
  • RIV/67985831:_____/11:00361401
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • cave sediments; chemical and physical properties; paleomagnetic analyses; Baiyun Cave (China) (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [98CCF467FD65]
http://linked.open...i/riv/mistoVydani
  • Postojna
http://linked.open...vEdiceCisloSvazku
  • Carsologica, 12
http://linked.open...i/riv/nazevZdroje
  • SOUTH CHINA KARST II
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...v/pocetStranKnihy
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Kogovšek, J.
  • Liu, H.
  • Pruner, Petr
  • Slabe, T.
  • Šebela, S.
http://linked.open...n/vavai/riv/zamer
number of pages
http://purl.org/ne...btex#hasPublisher
  • Inštitut za raziskovanjekrasa, ZRC SAZU=Karst Research Institute ZRC SAZU
https://schema.org/isbn
  • 978-961-254-241-2
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