Informace o publikaci
A vestige of very high - pressure (ca. 28 kbar) metamorphism in the Variscan Bohemian Massif, Czech Republic
| Autoři | |
|---|---|
| Rok publikování | 1997 |
| Druh | Článek v odborném periodiku |
| Časopis / Zdroj | European Journal of Mineralogy |
| Fakulta / Pracoviště MU | |
| Citace | |
| Obor | Geologie a mineralogie |
| Klíčová slova | garnetite; orthopyroxene; very-high pressure; Bohemian Massif |
| Popis | Pyropic garnetite from the Podolsko Complex, south Bohemian Moldanubian Zone, Bohemian Massif, records very-high pressure (28kbar, 830 deg.C)conditions of formation of the initial mineral assemblage. As such it represents the first evidence for very-high pressure metamorphism of continental crustal material in the Moldanubian Zone of the Bohemian Massif. This assemblage was extensively overprinted by complex symplectites, formed during a subsequent medium-pressure high-temperature event. |