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Magmatic and metasomatic processes in albite granites of the Vysoký Kámen cupola, Czech Republic

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    0207628 - USMH-B 20013049 RIV DE eng C - Conference Paper (international conference)
    Götze, J. - Kempe, U. - Wolf, D. - René, Miloš
    Magmatic and metasomatic processes in albite granites of the Vysoký Kámen cupola, Czech Republic.
    Cathodoluminescence in geosciences: New insight from CL in combination with other techniques. Freiberg: Technische Universität Bergakademie Freiberg, 2001, s. 106-107. ISBN 3-86012-151-0.
    [CL 2001. Freiberg (DE), 06.09.2001-08.09.2001]
    R&D Projects: GA MŠMT ME 364
    Institutional research plan: CEZ:AV0Z3046908
    Keywords : cathodoluminescence * topaz granite * geochemistry
    Subject RIV: DB - Geology ; Mineralogy

    The Vysoký Kámen stock is formed by medium-grained aplitic albite granite with typical peraluminous character and a strong negative europium anomaly. Intense metasomatic alteration of the primary granite resulted in irregular, mostly subhorizontal lenses and layers of younger feldspathites.
    Permanent Link: http://hdl.handle.net/11104/0103195

     
     

Number of the records: 1  

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