Molasse Basin-Carpathian Foredeep transition zone (AT/CZ) – T2.2. – In: Rupf, I., Diepolder, G.W. (ed.): Summary report of resources mapping and characterization, including descriptive reports on the case studies T2.1 - T2.10. - HotLime Deliverable 2.0: 130

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F20%3A00000436" target="_blank" >RIV/00025798:_____/20:00000436 - isvavai.cz</a>

Výsledek na webu

<a href="https://repository.europe-geology.eu/egdidocs/hotlime/hotlime_deliverable_20.pdf" target="_blank" >https://repository.europe-geology.eu/egdidocs/hotlime/hotlime_deliverable_20.pdf</a>

DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Molasse Basin-Carpathian Foredeep transition zone (AT/CZ) – T2.2. – In: Rupf, I., Diepolder, G.W. (ed.): Summary report of resources mapping and characterization, including descriptive reports on the case studies T2.1 - T2.10. - HotLime Deliverable 2.0: 130

Popis výsledku v původním jazyce

Upper Jurassic formations are mainly influenced by synthetic, SE-dipping normal faults with up to 700 m of vertical throw, creating depositional throughs for Mesozoic units, resulting in increased thickness close to fault zones. Antithetic, NW-dipping normal faults have only been detected in 2D seismic profiles in Czechia, exhibiting minor offsets of about 100 m. Alpine-Carpathian thrusts sheets do not affect the Upper Jurassic units in the modelling area. However, remnants of Jurassic strata from beneath the Vienna Basin further SE have been detached and transported to the surface within the frontal thrusts sheets of the Alpine-Carpathian Orogen and are now exposed in outcrops within the NE-SE striking Waschberg-Zdánice Zone.

Název v anglickém jazyce

Molasse Basin-Carpathian Foredeep transition zone (AT/CZ) – T2.2. – In: Rupf, I., Diepolder, G.W. (ed.): Summary report of resources mapping and characterization, including descriptive reports on the case studies T2.1 - T2.10. - HotLime Deliverable 2.0: 130

Popis výsledku anglicky

Upper Jurassic formations are mainly influenced by synthetic, SE-dipping normal faults with up to 700 m of vertical throw, creating depositional throughs for Mesozoic units, resulting in increased thickness close to fault zones. Antithetic, NW-dipping normal faults have only been detected in 2D seismic profiles in Czechia, exhibiting minor offsets of about 100 m. Alpine-Carpathian thrusts sheets do not affect the Upper Jurassic units in the modelling area. However, remnants of Jurassic strata from beneath the Vienna Basin further SE have been detached and transported to the surface within the frontal thrusts sheets of the Alpine-Carpathian Orogen and are now exposed in outcrops within the NE-SE striking Waschberg-Zdánice Zone.

Druh

O - Ostatní výsledky

CEP obor

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OECD FORD obor

10505 - Geology

Projekt

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Návaznosti

R - Projekt Ramcoveho programu EK

Rok uplatnění

2020

Kód důvěrnosti údajů

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