Abstract
The iron ore mineralizations at the Horni Benesov sulphidic deposit are located in the Devonian Sternberk - Horni Benesov Belt which is enveloped by the Lower Carboniferous flysch of the Culm Foreland Basin. The belt consists of metasedimentary and metavolcanic rocks. Horni Benesov is the only site in the Jeseniky Mountains, where the oxidic iron ores occur in close association with the sulphide orebodies of the VMS/SHMS type.
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