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

Kód výsledku v 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>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

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

Název v anglickém jazyce

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

Popis výsledku anglicky

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

Druh

D - Stať ve sborníku

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2001

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název statě ve sborníku

Abstracts of the 3rd Czech - Polish Workshop

ISBN

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ISSN

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e-ISSN

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Počet stran výsledku

1

Strana od-do

16

Název nakladatele

Institute of Rock Structure and Mechanics Academy of Science

Místo vydání

Ramzová

Místo konání akce

Ramzová

Datum konání akce

8. 11. 2001

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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