Pregled bibliografske jedinice broj: 210823
Siderite-hematite-barite-polysulfide mineral deposits, related to the early intra-continental Tethyan rifting, Inner Dinarides
Siderite-hematite-barite-polysulfide mineral deposits, related to the early intra-continental Tethyan rifting, Inner Dinarides // Proceedings of the Seventh Biennial SGA Meeting on Mineral Exploration and Sustainable Development / Eliopoulos, D.G.et al. (ur.).
Rotterdam : Boston (MA) : Taipei: Millpress Rotterdam, 2003. str. 1225-1229 (poster, nije recenziran, sažetak, znanstveni)
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Naslov
Siderite-hematite-barite-polysulfide mineral deposits, related to the early intra-continental Tethyan rifting, Inner Dinarides
Autori
Palinkaš, Ladislav ; Borojević, Sibila ; Strmić, Sabina ; Prochaska, Walter ; Spangenberg, J.
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Proceedings of the Seventh Biennial SGA Meeting on Mineral Exploration and Sustainable Development
/ Eliopoulos, D.G.et al. - Rotterdam : Boston (MA) : Taipei : Millpress Rotterdam, 2003, 1225-1229
ISBN
90-5966-015-3
Skup
Mineral Exploration and Sustainable Development
Mjesto i datum
Atena, Grčka, 24.08.2003. - 28.08.2003
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
Siderite-hematite-barite-polysulfide ore deposits; fluid inclusion chemistry; Pb.isotopes; S-isotopes; early intra-continental rifting; Inner Dinarides
Sažetak
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 Rožnava 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.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
