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Ti-rich granodiorite porphyries from the northeastern margin of the Klenov massif (Moldanubian Zone of the Bohemian Massif)

  1. 1.
    0208021 - USMH-B 20030110 RIV CZ eng J - Journal Article
    René, Miloš
    Ti-rich granodiorite porphyries from the northeastern margin of the Klenov massif (Moldanubian Zone of the Bohemian Massif).
    Acta Montana. Rada A, B. 23(130) (2003), s. 77-85. ISSN 1211-1910
    R&D Projects: GA ČR GA205/97/0514
    Institutional research plan: CEZ:AV0Z3046908
    Keywords : granodiorite porphyry * petrology * geochemistry
    Subject RIV: DB - Geology ; Mineralogy

    Ti-rich granodiorite porphyries from the northeastern margin of the Klenov massif are a part of the youngest magmatic activity of the Variscan magmatic phase in the Bohemian Massif. The examined granodiorite porphyries differ from other intermediate and basic dyke rocks of the Moldanubian Zone in their modal and geochemical composition and higher content of Ti-minerals.
    Permanent Link: http://hdl.handle.net/11104/0103582

     
     

Number of the records: 1  

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