Mineralogy and geochemistry of the bi-metasomatic contact zone between gneiss and marble from Žulová, Czech Republic
| Autoři | |
|---|---|
| Rok publikování | 2001 |
| Druh | Článek v odborném periodiku |
| Časopis / Zdroj | Mitteilungen der Österr. Mineral. Gesellschaft |
| Fakulta / Pracoviště MU | |
| Citace | |
| Obor | Geologie a mineralogie |
| Klíčová slova | contact mineralization; Žulová massif; bimetasomatic processes; contact metamorphism |
| Popis | The typical occurrences of contact zones - "tactites" between granitoids or gneisses and marbles in the area of Žulová massif were studied.The ratio between Fe2+ in pyroxens and Fe3+ in garnets of the contact zones indicates a reduction type of skarn with W-mineralization. |
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