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

The result's identifiers

  • Result code in 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>

  • Alternative codes found

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

  • Result on the web

    <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>

Alternative languages

  • Result language

    angličtina

  • Original language name

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

  • Original language 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, 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.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

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

Others

  • Publication year

    2015

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    International Journal of Earth Sciences

  • ISSN

    1437-3254

  • e-ISSN

  • Volume of the periodical

    104

  • Issue of the periodical within the volume

    4

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    28

  • Pages from-to

    963-990

  • UT code for WoS article

    000354949600003

  • EID of the result in the Scopus database