"RIV/00216224:14310/14:00080216" . . "B\u00E1bek, Ond\u0159ej" . "6"^^ . . . . "International Journal of Earth Sciences" . "33449" . . "The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians\u2019 foreland (NE Bohemian Massif)"@en . "DE - Spolkov\u00E1 republika N\u011Bmecko" . "The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians\u2019 foreland (NE Bohemian Massif)" . . "We give an interpretive review of the geological evolution of the Nysa-Morava Zone (NMZ)\u2014a Late Cenozoic tectonically active region of the NE Bohemian Massif located at its contact with the Western Carpathians\u2019 orogenic front. This crustal domain, delimited by generally NW\u2013SE-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\u2013SE-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\u2013Quaternary 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\u2013ESE and NW\u2013SE faults in a right-lateral transpressional setting."@en . "1"^^ . "We give an interpretive review of the geological evolution of the Nysa-Morava Zone (NMZ)\u2014a Late Cenozoic tectonically active region of the NE Bohemian Massif located at its contact with the Western Carpathians\u2019 orogenic front. This crustal domain, delimited by generally NW\u2013SE-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\u2013SE-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\u2013Quaternary 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\u2013ESE and NW\u2013SE faults in a right-lateral transpressional setting." . "Neuveden" . . . "The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians\u2019 foreland (NE Bohemian Massif)"@en . "1437-3254" . "Neuveden" . . . "14310" . "Sedl\u00E1\u010Dek, Jan" . . "RIV/00216224:14310/14:00080216!RIV15-MSM-14310___" . "\u0160t\u011Bpan\u010D\u00EDkov\u00E1, Petra" . . . . "P(GAP210/12/0573), P(LM2010008)" . "10.1007/s00531-014-1121-7" . "Bohemian Massif; Upper Morava Basin; Tectonic evolution; Seismicity; Sedimentary grabens; Late Cenozoic"@en . . "\u0160pa\u010Dek, Petr" . "Pazd\u00EDrkov\u00E1, Jana" . . "The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians\u2019 foreland (NE Bohemian Massif)" . "1"^^ . "\u0160vancara, Jan" . . . . "[32267B615447]" .