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Contrasting tectono-metamorphic evolution of orogenic lower crust in the Bohemian Massif: A numerical model

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F14%3A10133537" target="_blank" >RIV/00216208:11320/14:10133537 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/14:10133537 RIV/00025798:_____/14:00000015

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.gr.2012.08.020" target="_blank" >http://dx.doi.org/10.1016/j.gr.2012.08.020</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.gr.2012.08.020" target="_blank" >10.1016/j.gr.2012.08.020</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Contrasting tectono-metamorphic evolution of orogenic lower crust in the Bohemian Massif: A numerical model

  • Original language description

    The Bohemian Massif, located at the eastern margin of the European Variscan belt, is characterised by an exceptional accumulation of felsic high-pressure granulites. The petrological, structural and geochronological studies of this region revealed systematic differences between the tectonometamorphic evolution of the southern (Moldanubian) and northern (West Sudetes) parts of the orogen. Two contrasting tectonic scenarios have been proposed: gravity-driven vertical mass exchanges followed by continentalindentation in the Moldanubian domain, and crustal-scale folding leading to gneiss dome formation in the West Sudetes. We present a numerical model in order to correlate the apparent differences between these two regions with the variations in the dynamics of the modelled system. We model two colliding blocks: an orogenic root, where a felsic lower crust is overlain by a mafic layer and a middle crust, and a continental indentor. We examine the role of the rate of convergence of the two

  • 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

    S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2014

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Gondwana Research

  • ISSN

    1342-937X

  • e-ISSN

  • Volume of the periodical

    25

  • Issue of the periodical within the volume

    2

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    13

  • Pages from-to

    509-521

  • UT code for WoS article

    000333140600005

  • EID of the result in the Scopus database