Aplication of morphotectonic analysys for solving problems of structural conditions of uper silesian coal basin

Kód výsledku v IS VaVaI

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Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Aplication of morphotectonic analysys for solving problems of structural conditions of uper silesian coal basin

Popis výsledku v původním jazyce

The Upper Silesian coal basin is a suitable exemplary area where principles of morphotectonic analysis can be applied for solving problems of structural-tectonic conditions. The basin is a singular case by superimposition of three structural levels. Theoldest Cadomian level is represented by Brunovistulicum forming a forefield of Variscan accretion wedge represented by sediments of Rheno-Hercynian and Subvariscan (Upper Silesian coal basin) and at last Alpine accretion wedge formed by sediments of forearc basin and by Outer Carpathian nappes. The morphotectonic analysis is based on 3D visual interpretation of digital terrain models (DTM) of particular structural levels. Analysed digital models have been set up on basis of data from drilling and miningactivities, 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 DTM are confronted in view of mutual struc

Název v anglickém jazyce

Aplication of morphotectonic analysys for solving problems of structural conditions of uper silesian coal basin

Popis výsledku anglicky

The Upper Silesian coal basin is a suitable exemplary area where principles of morphotectonic analysis can be applied for solving problems of structural-tectonic conditions. The basin is a singular case by superimposition of three structural levels. Theoldest Cadomian level is represented by Brunovistulicum forming a forefield of Variscan accretion wedge represented by sediments of Rheno-Hercynian and Subvariscan (Upper Silesian coal basin) and at last Alpine accretion wedge formed by sediments of forearc basin and by Outer Carpathian nappes. The morphotectonic analysis is based on 3D visual interpretation of digital terrain models (DTM) of particular structural levels. Analysed digital models have been set up on basis of data from drilling and miningactivities, 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 DTM are confronted in view of mutual struc

Druh

D - Stať ve sborníku

CEP obor

DH - Báňský průmysl včetně těžby a zpracování uhlí

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2001

Kód důvěrnosti údajů

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

Název statě ve sborníku

COAL GEOLOGY CONFERENCE, PRAGUE 2001

ISBN

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ISSN

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e-ISSN

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Počet stran výsledku

1

Strana od-do

56

Název nakladatele

Coal Geology Conference

Místo vydání

Praha

Místo konání akce

Praha

Datum konání akce

25. 6. 2001

Typ akce podle státní příslušnosti

CST - Celostátní akce

Kód UT WoS článku

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