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Origin of felsic granulite microstructure by heterogeneous decomposition of alkali feldspar and extreme weakening of orogenic lower crust during the Variscan orogeny

  1. 1.
    SYSNO0357499
    TitleOrigin of felsic granulite microstructure by heterogeneous decomposition of alkali feldspar and extreme weakening of orogenic lower crust during the Variscan orogeny
    Author(s) Franěk, J. (CZ)
    Schulmann, K. (FR)
    Lexa, O. (CZ)
    Ulrich, Stanislav (GFU-E)
    Štípská, P. (FR)
    Haloda, J. (CZ)
    Týcová, P. (CZ)
    Source Title Journal of Metamorphic Geology. Roč. 29, č. 1 (2011), s. 103-130. - : Wiley
    Document TypeČlánek v odborném periodiku
    GrantGA205/05/2187, CZ - Czech Republic
    GA205/09/0539 GA ČR - Czech Science Foundation (CSF)
    CEZAV0Z30120515 - GFU-E (2005-2011)
    Languageeng
    CountryGB
    Keywords felsic granulites * Moldanubian domain * quantitative microstructural analysis * quartz and feldspar rheology * Variscan belt
    Permanent Linkhttp://hdl.handle.net/11104/0195763
     
Number of the records: 1  

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