
The Horní Benešov ore deposit in the Devonian Šternberk - Horní Benešov Belt, Jeseníky Mts, Czech Republic. Part 2: Fe - ore occurences
Autoři | |
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Rok publikování | 2013 |
Druh | Článek v odborném periodiku |
Časopis / Zdroj | Časopis Slezského muzea |
Citace | |
Doi | http://dx.doi.org/10.2478/cszma-2013-0023 |
Obor | Geologie a mineralogie |
Klíčová slova | Šternberk - Horní Benešov Belt, iron mineralization, mineralogy, fluid inclusions, stable isotopes, mineral-, whole rock- and REE- chemistry, genesis |
Popis | The iron ore mineralizations at the Horní Benešov sulphidic deposit are located in the Devonian Šternberk - Horní Benešov Belt which is enveloped by the Lower Carboniferous flysch of the Culm Foreland Basin. The belt consists of metasedimentary and metavolcanic rocks. Horní Benešov is the only site in the Jeseníky Mountains, where the oxidic iron ores occur in close association with the sulphide orebodies of the VMS/SHMS type. |