The impact of Outer Western Carpathian nappe tectonics on the recent stress-strain state in the Upper Silesian Coal Basin (Moravosilesian Zone, Bohemian Massif)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F12%3A00377039" target="_blank" >RIV/68145535:_____/12:00377039 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/61989100:27350/12:86083766

Výsledek na webu

<a href="http://versita.metapress.com/content/0326174t34663755/" target="_blank" >http://versita.metapress.com/content/0326174t34663755/</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.2478/v10096-012-0002-x" target="_blank" >10.2478/v10096-012-0002-x</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The impact of Outer Western Carpathian nappe tectonics on the recent stress-strain state in the Upper Silesian Coal Basin (Moravosilesian Zone, Bohemian Massif)

Popis výsledku v původním jazyce

The Upper Silesian Coal Basin (USCB) represents a typical foreland basin developed during the Variscan orogenic phase of the Late Carboniferous. Later, during the Alpine orogeny the Outer Western Carpathian nappes were thrust over the post-Variscan foreland, to which the USCB belongs.Due to this complex tectonic history, redistribution of stress fields occurred in the post-Variscan basement. Furthermore,post-Variscan denudation processes probably also contributed to recent stress regimes.Nevertheless, the impact of the West Carpathian orogeny can be regarded as the most significant influence.The in-situ measurement of recent stress fields in deposits of the Karvina Formation of the USCB and structural analysis of the Czech part of the USCB, has focusedon verification of the structure and stress interference of the Carpathian nappes and post-Variscan foreland basement.In the southernmost part of the Karvina Subbasin, the easternmost domain of the USCB,situated in the apical zone of the

Název v anglickém jazyce

The impact of Outer Western Carpathian nappe tectonics on the recent stress-strain state in the Upper Silesian Coal Basin (Moravosilesian Zone, Bohemian Massif)

Popis výsledku anglicky

The Upper Silesian Coal Basin (USCB) represents a typical foreland basin developed during the Variscan orogenic phase of the Late Carboniferous. Later, during the Alpine orogeny the Outer Western Carpathian nappes were thrust over the post-Variscan foreland, to which the USCB belongs.Due to this complex tectonic history, redistribution of stress fields occurred in the post-Variscan basement. Furthermore,post-Variscan denudation processes probably also contributed to recent stress regimes.Nevertheless, the impact of the West Carpathian orogeny can be regarded as the most significant influence.The in-situ measurement of recent stress fields in deposits of the Karvina Formation of the USCB and structural analysis of the Czech part of the USCB, has focusedon verification of the structure and stress interference of the Carpathian nappes and post-Variscan foreland basement.In the southernmost part of the Karvina Subbasin, the easternmost domain of the USCB,situated in the apical zone of the

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GA105%2F08%2F1625" target="_blank" >GA105/08/1625: Vývoj napěťových polí v horském masivu na základě paleonapěťové analýzy tektonických procesů v české části hornoslezské pánve</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2012

Kód důvěrnosti údajů

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

Název periodika

Geologica Carpathica

ISSN

1335-0552

e-ISSN

—

Svazek periodika

63

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

SK - Slovenská republika

Počet stran výsledku

10

Strana od-do

3-11

Kód UT WoS článku

000301748900001

EID výsledku v databázi Scopus

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