Recent-stress state in Czech part of Upper Silesian Coal basin

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F09%3A00332343" target="_blank" >RIV/68145535:_____/09:00332343 - 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

Recent-stress state in Czech part of Upper Silesian Coal basin

Popis výsledku v původním jazyce

Knowledge of stress strain fields and their development is the fudamental for all mine working and for its right planing most importantly in the rock burst risk regions. A model of stresses causing Variscan structural tectonic pattern in the Czech part of Upper Silesian Coal Basin (USCB) based on paleostress analyse have been interpreted. It was compiled used many of tectonic measurements of planar and linear elements and comparison with the knowledge of dynamic development of Variscan body in a largerframework of Moravo Silesian zone. It was took account the influence of Alpine deformation due to Karpatian nappes. There were more stress tensor gauging realised in the region above all using hydrofrac and treated overcoring methods during last ten years. It?s becoming apparent that for information of recent stress fields is usable the interpretation of focus mechanisms of energetic significant seismic events, which were observed here more than ten years.

Název v anglickém jazyce

Recent-stress state in Czech part of Upper Silesian Coal basin

Popis výsledku anglicky

Knowledge of stress strain fields and their development is the fudamental for all mine working and for its right planing most importantly in the rock burst risk regions. A model of stresses causing Variscan structural tectonic pattern in the Czech part of Upper Silesian Coal Basin (USCB) based on paleostress analyse have been interpreted. It was compiled used many of tectonic measurements of planar and linear elements and comparison with the knowledge of dynamic development of Variscan body in a largerframework of Moravo Silesian zone. It was took account the influence of Alpine deformation due to Karpatian nappes. There were more stress tensor gauging realised in the region above all using hydrofrac and treated overcoring methods during last ten years. It?s becoming apparent that for information of recent stress fields is usable the interpretation of focus mechanisms of energetic significant seismic events, which were observed here more than ten years.

Druh

D - Stať ve sborníku

CEP obor

DH - Báňský průmysl včetně těžby a zpracování uhlí

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

2009

Kód důvěrnosti údajů

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

Název statě ve sborníku

Górnicze zagrozenia naturalne 2009 /16./

ISBN

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ISSN

1643-7608

e-ISSN

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Počet stran výsledku

9

Strana od-do

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Název nakladatele

Glowny Instytut Górnictwa

Místo vydání

Katowice

Místo konání akce

Andrzychów

Datum konání akce

3. 11. 2009

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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