Publication details
Origin of the Zálesí U-Ni-Co-As-Ag/Bi deposit, Bohemian Massif, Czech Republic: Fluid inclusion and stable isotope constraints
| Authors | |
|---|---|
| Year of publication | 2009 |
| Type | Article in Periodical |
| Magazine / Source | Mineralium Deposita |
| MU Faculty or unit | |
| Citation | |
| Doi | https://doi.org/10.1007/s00126-008-0202-6 |
| Field | Geology and mineralogy |
| Keywords | Bohemian Massif; Zálesí; Czech Republic; Five-element association; Uranium; Fluid inclusions; Stable isotopes |
| Description | 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. |