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Description
  • Moravský kras je tvořen vápenci, v jejichž podloží vystupují terestrická siliciklastika a proterozoické granitoidy (západně). Východně, severně a jižně od vápenců v jejich nadloží vystupují spodnokarbonská mořská siliciklastika kulmské facie. Usazování vápenců započalo ve středním devonu a skončilo ve spodním karbonu. Záznam paleokrasových jevů je znám ze středního devonu, spodního karbonu, svrchní jury, spodní křídy a miocénu. (cs)
  • Moravian karst is a carbonate area surrounded with underlying terrestric siliciclastcs and Proterozoic granitoids at the west and with overlying Lower Carboniferous turbidite siliciclastics of the Culm facies at the north, east and south. The deposiliton of carbonates started in Middle Devonian and finished in Lower Carboniferous. Records of paleokarst phenomena are known from the Middle Devonian, Lower Carboniferous, Upper Jurassic, Lower Cretaceous ad Miocene.
  • Moravian karst is a carbonate area surrounded with underlying terrestric siliciclastcs and Proterozoic granitoids at the west and with overlying Lower Carboniferous turbidite siliciclastics of the Culm facies at the north, east and south. The deposiliton of carbonates started in Middle Devonian and finished in Lower Carboniferous. Records of paleokarst phenomena are known from the Middle Devonian, Lower Carboniferous, Upper Jurassic, Lower Cretaceous ad Miocene. (en)
Title
  • Introduction to geology and paleokarst history of the Moravian Karst
  • Úvod do geologie a paleokrasové historie Moravského krasu (cs)
  • Introduction to geology and paleokarst history of the Moravian Karst (en)
skos:prefLabel
  • Introduction to geology and paleokarst history of the Moravian Karst
  • Úvod do geologie a paleokrasové historie Moravského krasu (cs)
  • Introduction to geology and paleokarst history of the Moravian Karst (en)
skos:notation
  • RIV/00025798:_____/07:00000373!RIV08-MZP-00025798
http://linked.open.../vavai/riv/strany
  • 31-36
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(MZP0002579801)
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
  • 427388
http://linked.open...ai/riv/idVysledku
  • RIV/00025798:_____/07:00000373
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Devonian, carbonate platform, paleokarst, spelogenesis (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [9830FFDCAE13]
http://linked.open...v/mistoKonaniAkce
  • Brno
http://linked.open...i/riv/mistoVydani
  • Brno
http://linked.open...i/riv/nazevZdroje
  • Scripta Facultatis Scientiarum Naturalium Universitatis Masarykianae Brunensis.Geology
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Otava, Jiří
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
http://linked.open...n/vavai/riv/zamer
number of pages
http://purl.org/ne...btex#hasPublisher
  • Masarykova univerzita
https://schema.org/isbn
  • 978-80-210-4368-8
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