Informace o publikaci
Origin of the Zálesí U-Ni-Co-As-Ag/Bi deposit, Bohemian Massif, Czech Republic: Fluid inclusion and stable isotope constraints
| Autoři | |
|---|---|
| Rok publikování | 2009 |
| Druh | Článek v odborném periodiku |
| Časopis / Zdroj | Mineralium Deposita |
| Fakulta / Pracoviště MU | |
| Citace | DOLNÍČEK, Zdeněk, Bohuslav FOJT, Walter PROCHASKA, Jan KUČERA a Petr SULOVSKÝ. Origin of the Zálesí U-Ni-Co-As-Ag/Bi deposit, Bohemian Massif, Czech Republic: Fluid inclusion and stable isotope constraints. Mineralium Deposita. 2009, roč. 44, č. 1, s. 81-97. ISSN 0026-4598. Dostupné z: https://dx.doi.org/10.1007/s00126-008-0202-6. |
| Doi | http://dx.doi.org/10.1007/s00126-008-0202-6 |
| Obor | Geologie a mineralogie |
| Klíčová slova | Bohemian Massif; Zálesí; Czech Republic; Five-element association; Uranium; Fluid inclusions; Stable isotopes |
| Popis | Abstract The Zálesí vein-type deposit is hosted by Early Paleozoic high-grade metamorphic rocks on the northern margin of the Bohemian Massif. The mineralization is composed of three main stages: uraninite, arsenide, and sulfide. The mineral assemblages formed at low temperatures and low pressures. |