Approximation of the missing eroded sediments in the Bílé Karpaty Unit (Outer West Carpathians)

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F04%3A00002394" target="_blank" >RIV/61989592:15310/04:00002394 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Approximation of the missing eroded sediments in the Bílé Karpaty Unit (Outer West Carpathians)
Original language description
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.
Czech name
Odhad chybějících erodovaných sedimentů bělokarpatské jednotky
Czech description
V článku je detailně geologicky mapován odhad chybějících erodovaných sedimentů bělokarpatské jednotky.

Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DE - Earth magnetism, geodesy, geography
OECD FORD branch
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Project
<a href="/en/project/GA205%2F03%2F0211" target="_blank" >GA205/03/0211: Geography of selected natural extremes, their impacts and cartographic visualisation in Moravia and Silesia</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2004
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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