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An Entity of Type : http://linked.opendata.cz/ontology/domain/vavai/Vysledek, within Data Space : linked.opendata.cz associated with source document(s)

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Description
  • Křemitý, železitý a karbonátový tmel jsou nejčastějšími sekundárními složkami pískovců a často zcela vyplňují mezizrnové prostory. Přítomnost tmelu vyžaduje existenci zdroje příslušných prvků uvnitř nebo vně pánve, mobilizaci fluid příznivého chemického složení, pH a teploty schopných transportu těchto prvků, a podmínky v pánvi, za nichž jsou novotvořené minerály stabilní. Vešketé druhy tmelu mají vliv na paleohydraulické vlastonsti pískovcového masivu a ovlivňují tvorbu specifických tvarů zvětrávání a odnosu. (cs)
  • Siliceous, ferruginous and carbonate cements are the most common secondary constituents of sandstones, often completely filling all intergranular spaces. The presence of mineral cement necessitates an intra- or extrabasinal source of the elements needed, mobilization of fluids of appropriate chemistry, pH, and temperature to transport these elements, and finally, an establishment of conditions within the stability window of the particular cementing minerals in the sedimentary basin or its part. All types of cement control paleohydraulic properties of the sandstone massif as well as the formation of specific landforms.
  • Siliceous, ferruginous and carbonate cements are the most common secondary constituents of sandstones, often completely filling all intergranular spaces. The presence of mineral cement necessitates an intra- or extrabasinal source of the elements needed, mobilization of fluids of appropriate chemistry, pH, and temperature to transport these elements, and finally, an establishment of conditions within the stability window of the particular cementing minerals in the sedimentary basin or its part. All types of cement control paleohydraulic properties of the sandstone massif as well as the formation of specific landforms. (en)
Title
  • Sandstone cementation and its geomorphic and hydraulic implications
  • Cementace pískovců a její geomorfologické a hydraulické důsledky (cs)
  • Sandstone cementation and its geomorphic and hydraulic implications (en)
skos:prefLabel
  • Sandstone cementation and its geomorphic and hydraulic implications
  • Cementace pískovců a její geomorfologické a hydraulické důsledky (cs)
  • Sandstone cementation and its geomorphic and hydraulic implications (en)
skos:notation
  • RIV/67985831:_____/05:00028556!RIV06-AV0-67985831
http://linked.open.../vavai/riv/strany
  • 21;24
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IAA3013302), Z(AV0Z30130516)
http://linked.open...iv/cisloPeriodika
  • -
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
  • 541865
http://linked.open...ai/riv/idVysledku
  • RIV/67985831:_____/05:00028556
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • sandstone; paleohydraulics; geomorphology; siliceous cement; carbonate cement; ferruginous cement; sandstone landsforms (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • LU - Lucemburské velkovévodství
http://linked.open...ontrolniKodProRIV
  • [811EA72EB9E9]
http://linked.open...i/riv/nazevZdroje
  • Ferrantia : travaux scientifiques du Musée national d'histoire naturelle de Luxembourg
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 44
http://linked.open...iv/tvurceVysledku
  • Adamovič, Jiří
http://linked.open...n/vavai/riv/zamer
issn
  • 1682-5519
number of pages
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