Podrobnosti záznamu

    The Brno Batholith: an insight into the magmatic and metamorphic evolution of the Cadomian Brunovistulian Unit,eastern margin of the Bohemian Massif
    Hoeck, Volker
    Leichmann, Jaromír
Typ dokumentu
    článek v periodiku
Zdrojový dokument - seriál
    Journal of Geosciences
    Roč. 53, č. 1
Výraz tezauru
    Brno Batholith
Klíčové slovo
Abstrakt (anglicky)
   The Brno Batholith, a part of the larger Brunovistulian Unit, consists of three genetically independent complexes, Western Granitoid Complex (part of the Thaya Terrane), Ophiolite Belt (formerly Metabasite Zone or Central Basic Belt), and Eastern Granitoid Complex (part of the Slavkov Terrane). The field with geochronological evidence indicate younger age of both granitoid complexes compared with the ophiolite. The composition of the Eastern Granitoid Complex (not newly studied in this paper) points to a relatively primitive Cadomian volcanic-arc environment. The Ophiolite Belt comprises a tilted segment of an almost complete metamorphosed ophiolite sequence with lithologically and geochemically obvious suprasubduction signature. Three main granite suites, with distinct S, I, and A type affinities, are exposed in the Western Granitoid Complex.
    MU Brno, Přírodovědecká fakulta
Kód přispěvatele
    MU, PřF
Zdrojový formát
Datum importu
    8. 8. 2012