Interaction between Alpine and Vatican orogeny on the Basis os study digital elevation models - Moravosilesian area

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F01%3A00000089" target="_blank" >RIV/61989100:27350/01:00000089 - 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
Interaction between Alpine and Vatican orogeny on the Basis os study digital elevation models - Moravosilesian area
Original language description
The Moravosilesian area of the Bohemian Massif is right area where principles of morphotectonic analysis can be applied for solving problem of structural-tectonic conditions. The area is singular case by superposition of three structural levels. Lower most Pan-African (Cadomian) Brunovistulicum foreland terrane played an essential role in development of Variscan accretion wedge represented by sediments of Rheno-Hercynian foredeep and Subvariscan foreland basin. At last Alpine accretion wedge formed by sediments of foredeep basin and Outer Carpatian nappes. The morphotectonic analysis is based on 3D visual interpretation of digital elevation models (DEM) of above-mentioned particular structural levels. Analysed digital models have been set up on basisofdata from drilling and mining activities, of satellite radar data, of data from geophysical seismic and magnetometric survey, especially however from detailed digitalisation of topographic map of 1 : 25 000 scale. Particular DEM are conf
Czech name
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Czech description
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Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2001
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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