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Description
  • V článku je detailně geologicky mapován odhad chybějících erodovaných sedimentů bělokarpatské jednotky. (cs)
  • The erosion of up to 1,400 m of the rock column in the Bílé Karpaty Unit (Magura Nappe, Czech Republic) since the Sarmatian is inferred on the basis of anisotropy of magnetic susceptibility (AMS), vitrinite reflection analysis, rock-eval analysis, K/Ar radiometric dating, and detailed geological mapping. The erosion of nearly 1.5 km of rocks since the Sarmatian contradicts the idea of the presence of planation surfaces of Sarmatian age in this part of the Outer West Carpathians. Evolution of the topography has probably been the result of dynamic equilibrium between uplift and erosion. Thus, the present-day topography should be young, as indicated by the fact that the oldest dated landslides are no older than 13,000 years BP.
  • The erosion of up to 1,400 m of the rock column in the Bílé Karpaty Unit (Magura Nappe, Czech Republic) since the Sarmatian is inferred on the basis of anisotropy of magnetic susceptibility (AMS), vitrinite reflection analysis, rock-eval analysis, K/Ar radiometric dating, and detailed geological mapping. The erosion of nearly 1.5 km of rocks since the Sarmatian contradicts the idea of the presence of planation surfaces of Sarmatian age in this part of the Outer West Carpathians. Evolution of the topography has probably been the result of dynamic equilibrium between uplift and erosion. Thus, the present-day topography should be young, as indicated by the fact that the oldest dated landslides are no older than 13,000 years BP. (en)
Title
  • Approximation of the missing eroded sediments in the Bílé Karpaty Unit (Outer West Carpathians)
  • Approximation of the missing eroded sediments in the Bílé Karpaty Unit (Outer West Carpathians) (en)
  • Odhad chybějících erodovaných sedimentů bělokarpatské jednotky (cs)
skos:prefLabel
  • Approximation of the missing eroded sediments in the Bílé Karpaty Unit (Outer West Carpathians)
  • Approximation of the missing eroded sediments in the Bílé Karpaty Unit (Outer West Carpathians) (en)
  • Odhad chybějících erodovaných sedimentů bělokarpatské jednotky (cs)
skos:notation
  • RIV/61989592:15310/04:00002394!RIV/2005/GA0/153105/N
http://linked.open.../vavai/riv/strany
  • 59-66
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA205/03/0211)
http://linked.open...iv/cisloPeriodika
  • 1
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
  • 555273
http://linked.open...ai/riv/idVysledku
  • RIV/61989592:15310/04:00002394
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • topographic evolution;denudation;planation surfaces;geochemical analysis of rocks;Magura Nappe (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • PL - Polská republika
http://linked.open...ontrolniKodProRIV
  • [8DD8C6134C23]
http://linked.open...i/riv/nazevZdroje
  • Studia Geomorphologica Carpatho-Balcanica
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
  • 38
http://linked.open...iv/tvurceVysledku
  • Přichystal, A.
  • Hrouda, F.
  • Franců, J.
  • Krejčí, O.
  • Bíl, Martin
issn
  • 0081-6434
number of pages
http://localhost/t...ganizacniJednotka
  • 15310
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