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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 | |
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Rok publikování | 2009 |
Druh | Článek v odborném periodiku |
Časopis / Zdroj | Mineralium Deposita |
Fakulta / Pracoviště MU | |
Citace | |
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. |