About: Depositional environment of the %22Old Red%22 sediments in the Brno area (South-eastern part of the Rhenohercynian zone, Bohemian Massif)     Goto   Sponge   NotDistinct   Permalink

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Description
  • Lower Devonian monomict-quartzose coarse-grained clastics are interpreted as the deposits of an alluvial fan built up mainly by catastrophic sheetfloods. The main sources were probably granites and gneisses, other components were derived from rhyolites, older siliciclastics sediments and low-grade metamorphic rocks. Rapid uplift, erosion dominated by mechanical weathering and multiple redeposition are supposed within the drainage basin. The flat alluvial fan was only slightly reworked and eroded during subsequent non-catastrophic overland flows (sedondary processes).
  • Lower Devonian monomict-quartzose coarse-grained clastics are interpreted as the deposits of an alluvial fan built up mainly by catastrophic sheetfloods. The main sources were probably granites and gneisses, other components were derived from rhyolites, older siliciclastics sediments and low-grade metamorphic rocks. Rapid uplift, erosion dominated by mechanical weathering and multiple redeposition are supposed within the drainage basin. The flat alluvial fan was only slightly reworked and eroded during subsequent non-catastrophic overland flows (sedondary processes). (en)
Title
  • Depositional environment of the %22Old Red%22 sediments in the Brno area (South-eastern part of the Rhenohercynian zone, Bohemian Massif)
  • Depositional environment of the %22Old Red%22 sediments in the Brno area (South-eastern part of the Rhenohercynian zone, Bohemian Massif) (en)
skos:prefLabel
  • Depositional environment of the %22Old Red%22 sediments in the Brno area (South-eastern part of the Rhenohercynian zone, Bohemian Massif)
  • Depositional environment of the %22Old Red%22 sediments in the Brno area (South-eastern part of the Rhenohercynian zone, Bohemian Massif) (en)
skos:notation
  • RIV/00216224:14310/01:00004419!RIV/2002/MSM/143102/N
http://linked.open.../vavai/riv/strany
  • 195
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(MSM 143100004)
http://linked.open...iv/cisloPeriodika
  • 4
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
  • 677157
http://linked.open...ai/riv/idVysledku
  • RIV/00216224:14310/01:00004419
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Early Paleozoic, monomict-quartzose clastics, conglomerates, sheetfloods (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • SK - Slovenská republika
http://linked.open...ontrolniKodProRIV
  • [228C560B0342]
http://linked.open...i/riv/nazevZdroje
  • Geologica Carpathica
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...ocetUcastnikuAkce
http://linked.open...nichUcastnikuAkce
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 52
http://linked.open...iv/tvurceVysledku
  • Kalvoda, Jiří
  • Leichmann, Jaromír
  • Nehyba, Slavomír
http://linked.open...n/vavai/riv/zamer
issn
  • 1335-0552
number of pages
http://localhost/t...ganizacniJednotka
  • 14310
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