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.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
