The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians? foreland (NE Bohemian Massif)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F15%3A00080786" target="_blank" >RIV/00216224:14310/15:00080786 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985891:_____/15:00449424 RIV/61989592:15310/15:33157348

Výsledek na webu

<a href="http://dx.doi.org/10.1007/s00531-014-1121-7" target="_blank" >http://dx.doi.org/10.1007/s00531-014-1121-7</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s00531-014-1121-7" target="_blank" >10.1007/s00531-014-1121-7</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians? foreland (NE Bohemian Massif)

Popis výsledku v původním jazyce

We give an interpretive review of the geological evolution of the Nysa-Morava Zone (NMZ)?a Late Cenozoic tectonically active region of the NE Bohemian Massif located at its contact with the Western Carpathians? orogenic front. This crustal domain, delimited by generally NW?SE-striking fault system, is characterised by Oligo-Miocene and Plio-Pleistocene volcanic activity, regionally anomalous, weak historical and present-day seismicity and increased CO2 flux. The NMZ hosts several elongated, mostly NW?SE-trending, graben-like sedimentary basins (Upper Morava Basin System), which are filled by more than 300-m-thick succession of clastic fluvial/lacustrine sediments of Pliocene?Quaternary age. Based on geometric relations, basin architecture, coincidenceof seismicity with CO2 escape and sparse focal mechanism data, a model is proposed, which explains this active domain as a transfer zone developed between major WNW?ESE and NW?SE faults in a right-lateral transpressional setting.

Název v anglickém jazyce

The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians? foreland (NE Bohemian Massif)

Popis výsledku anglicky

We give an interpretive review of the geological evolution of the Nysa-Morava Zone (NMZ)?a Late Cenozoic tectonically active region of the NE Bohemian Massif located at its contact with the Western Carpathians? orogenic front. This crustal domain, delimited by generally NW?SE-striking fault system, is characterised by Oligo-Miocene and Plio-Pleistocene volcanic activity, regionally anomalous, weak historical and present-day seismicity and increased CO2 flux. The NMZ hosts several elongated, mostly NW?SE-trending, graben-like sedimentary basins (Upper Morava Basin System), which are filled by more than 300-m-thick succession of clastic fluvial/lacustrine sediments of Pliocene?Quaternary age. Based on geometric relations, basin architecture, coincidenceof seismicity with CO2 escape and sparse focal mechanism data, a model is proposed, which explains this active domain as a transfer zone developed between major WNW?ESE and NW?SE faults in a right-lateral transpressional setting.

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

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název periodika

International Journal of Earth Sciences

ISSN

1437-3254

e-ISSN

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Svazek periodika

104

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

28

Strana od-do

963-990

Kód UT WoS článku

000354949600003

EID výsledku v databázi Scopus

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