Structural Geology Research of the Sudoměřice Tunnel ? the Paleostress Analysis (Moldanubicum, South Bohemia)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F15%3A00082891" target="_blank" >RIV/00216224:14310/15:00082891 - 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

Structural Geology Research of the Sudoměřice Tunnel ? the Paleostress Analysis (Moldanubicum, South Bohemia)

Popis výsledku v původním jazyce

The study area is located in the central part of the Moldanubicum, in the Variegated Unit. It is bordered by the Mid-Bohemian Plutonic complex in the west. Data were collected from new Sudoměřice tunnel excavation, recently excavated outcrops and naturaloutcrops tunnel construction surroundings. Double track Sudoměřice tunnel is part of the Tábor ? Sudoměřice u Tábora railway track section of 4th railway transit corridor Praha ? České Budějovice. The tunnel excavation proceeded through biotite-sillimanit paragneiss and migmatite with sporadic fine-grained aplite intrusions. Paragneiss and migmatite are medium to fine-grained with distinctive W-E foliation dipping 10?30° to the north. Rock was variously altered along faults and joints. Similar geologywas documented in other studied localities (old track cuts, recently excavated cuts for new track, excavated outcrop for new underpass to Sudoměřice station, outcrops west of Prudice, near D3 motorway, and Moraveč).

Název v anglickém jazyce

Structural Geology Research of the Sudoměřice Tunnel ? the Paleostress Analysis (Moldanubicum, South Bohemia)

Popis výsledku anglicky

The study area is located in the central part of the Moldanubicum, in the Variegated Unit. It is bordered by the Mid-Bohemian Plutonic complex in the west. Data were collected from new Sudoměřice tunnel excavation, recently excavated outcrops and naturaloutcrops tunnel construction surroundings. Double track Sudoměřice tunnel is part of the Tábor ? Sudoměřice u Tábora railway track section of 4th railway transit corridor Praha ? České Budějovice. The tunnel excavation proceeded through biotite-sillimanit paragneiss and migmatite with sporadic fine-grained aplite intrusions. Paragneiss and migmatite are medium to fine-grained with distinctive W-E foliation dipping 10?30° to the north. Rock was variously altered along faults and joints. Similar geologywas documented in other studied localities (old track cuts, recently excavated cuts for new track, excavated outcrop for new underpass to Sudoměřice station, outcrops west of Prudice, near D3 motorway, and Moraveč).

Druh

O - Ostatní výsledky

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2015

Kód důvěrnosti údajů

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