Siderite-hematite-barite-polysulfide mineral deposits, related to the early intra-continental Tethyan rifting, Inner Dinarides

摘要

Permian siderite-barite-hematite-polysulfide (SBHD) mineral deposits placed at the margin of the Mesozoic carbonate platform and along Inner Dinarides demarcate opening of the Tethys. There is a long array of deposits from NW Monte Negro, Central Bosnia, Ljubija, Trgovska gora and Petrova gora following the general SE-NW Dinaric lineaments. The deposits of similar genetic style, Rude-Samoborska Gora, Bistra-Medvednica, Rudabanya (Hungary) accommodate along the Zagorje-Mid-Transdanubian zone (ZMT), a northeastern extention of the Internal Dinarides, stretching SW-NE, and terminates within Gemerides with Rudnyani and Roznava in Slovakia. Beside geological and paragenetical similarity, there is an ever increasing record on fluid inclusion P,T,X characteristics and radiogenic and stable isotope data which unambiguously confirm their unique geotectonic and genetic heritage affiliated to the Early intra-continental rifting of the Tethys.