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Very-high pressure Variscan metamorphism in the Gföhl Unit, south-central Bohemia: Evidence from crustal pyropic garnetite.
Autoři | |
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Rok publikování | 1999 |
Druh | Článek v odborném periodiku |
Časopis / Zdroj | Journal of Conference Abstracts |
Fakulta / Pracoviště MU | |
Citace | |
Obor | Geologie a mineralogie |
Klíčová slova | pyropic garnetite; zircon; monazite; U-Pb dating; Variscan metamorphism; Gfohl Unit; Bohemian Massif |
Popis | Zircon and monazite U-Pb ages for pyropic garnetite from south Bohemian Moldanubian zone are presented as evidence for very-high pressure Variscan metamorphism in the Gfohl unit. |