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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F14%3A00080216%21RIV15-MSM-14310___
rdf:type
n12:Vysledek skos:Concept
dcterms:description
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, coincidence of 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. 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, coincidence of 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.
dcterms:title
The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians’ foreland (NE Bohemian Massif) The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians’ foreland (NE Bohemian Massif)
skos:prefLabel
The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians’ foreland (NE Bohemian Massif) The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians’ foreland (NE Bohemian Massif)
skos:notation
RIV/00216224:14310/14:00080216!RIV15-MSM-14310___
n3:aktivita
n6:P
n3:aktivity
P(GAP210/12/0573), P(LM2010008)
n3:cisloPeriodika
Neuveden
n3:dodaniDat
n7:2015
n3:domaciTvurceVysledku
n8:7162286
n3:druhVysledku
n18:J
n3:duvernostUdaju
n10:S
n3:entitaPredkladatele
n4:predkladatel
n3:idSjednocenehoVysledku
33449
n3:idVysledku
RIV/00216224:14310/14:00080216
n3:jazykVysledku
n19:eng
n3:klicovaSlova
Bohemian Massif; Upper Morava Basin; Tectonic evolution; Seismicity; Sedimentary grabens; Late Cenozoic
n3:klicoveSlovo
n5:Late%20Cenozoic n5:Upper%20Morava%20Basin n5:Tectonic%20evolution n5:Seismicity n5:Sedimentary%20grabens n5:Bohemian%20Massif
n3:kodStatuVydavatele
DE - Spolková republika Německo
n3:kontrolniKodProRIV
[32267B615447]
n3:nazevZdroje
International Journal of Earth Sciences
n3:obor
n15:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
6
n3:projekt
n16:LM2010008 n16:GAP210%2F12%2F0573
n3:rokUplatneniVysledku
n7:2014
n3:svazekPeriodika
Neuveden
n3:tvurceVysledku
Bábek, Ondřej Sedláček, Jan Štěpančíková, Petra Špaček, Petr Pazdírková, Jana Švancara, Jan
s:issn
1437-3254
s:numberOfPages
1
n17:doi
10.1007/s00531-014-1121-7
n14:organizacniJednotka
14310