Exhumované tvary kenozoického stáří na jihovýchodním úbočí Českého masivu v České republice a Rakousku

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F05%3A00025406" target="_blank" >RIV/68145535:_____/05:00025406 - 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

Exhumed Cenozoic landforms on the SE flank of the Bohemian Massif in the Czech Republic and Austria

Popis výsledku v původním jazyce

Exhumed Cenozoic landforms situated on the marginal slope of the Bohemian Massif in the contact area with the Alpine-Carpathian Foredeep in S Moravia (Czech Republic) and N Lower Austria are described. Small elongated crystalline ridges and inselberg-like hills surrounded by Lower Miocene marine clastic deposits are characteristic for the region. The tightly oriented bedrock pattern was predisposed by its position along an old fault zone. The horst-and-graben topography in the present-day landscape of the area evolved within the marginal downwarp of the Bohemian Massif in the Cenozoic, caused by Alpine orogenic movements in the Eastern Alps and Western Carpathians. In the lower Neogene, several transgressions with high rates of sedimentation on the flank of the Massif were connected with the tectonic processes. From the upper Neogene to the Quaternary the subsidence regime was replaced by significant regional uplift, accompanied by intensive denudation of weakly consolidated young d...

Název v anglickém jazyce

Exhumed Cenozoic landforms on the SE flank of the Bohemian Massif in the Czech Republic and Austria

Popis výsledku anglicky

Exhumed Cenozoic landforms situated on the marginal slope of the Bohemian Massif in the contact area with the Alpine-Carpathian Foredeep in S Moravia (Czech Republic) and N Lower Austria are described. Small elongated crystalline ridges and inselberg-like hills surrounded by Lower Miocene marine clastic deposits are characteristic for the region. The tightly oriented bedrock pattern was predisposed by its position along an old fault zone. The horst-and-graben topography in the present-day landscape of the area evolved within the marginal downwarp of the Bohemian Massif in the Cenozoic, caused by Alpine orogenic movements in the Eastern Alps and Western Carpathians. In the lower Neogene, several transgressions with high rates of sedimentation on the flank of the Massif were connected with the tectonic processes. From the upper Neogene to the Quaternary the subsidence regime was replaced by significant regional uplift, accompanied by intensive denudation of weakly consolidated young d...

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

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2005

Kód důvěrnosti údajů

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

Název periodika

Zeitschrift für Geomorphologie

ISSN

0372-8854

e-ISSN

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Svazek periodika

49

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

22

Strana od-do

23-45

Kód UT WoS článku

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EID výsledku v databázi Scopus

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