Multiphase formation of the Obří důl polymetallic skarn deposit, West Sudetes, Bohemian Massif: geochemistry and Re–Os dating of sulfide mineralization

0489612 - GLÚ 2019 RIV DE eng J - Článek v odborném periodiku
Veselovský, F. - Ackerman, Lukáš - Pašava, J. - Žák, Karel - Haluzová, Eva - Creaser, R. A. - Dobeš, P. - Erban, V. - Tásler, R.
Multiphase formation of the Obří důl polymetallic skarn deposit, West Sudetes, Bohemian Massif: geochemistry and Re–Os dating of sulfide mineralization.
Mineralium deposita. Roč. 53, č. 5 (2018), s. 665-682. ISSN 0026-4598. E-ISSN 1432-1866
Grant CEP: GA ČR GA13-15390S
Institucionální podpora: RVO:67985831
Klíčová slova: Bohemian Massif * polymetallic skarn deposit * West Sudetes * arsenopyrite * Re–Os geochronology
Obor OECD: Geology
Impakt faktor: 3.397, rok: 2018

The Obří důl Fe–Cu–As polymetallic sulfide skarn deposit is developed in a metamorphic series in the West Sudetes, Bohemian Massif. It consists of lenses of marble, calc–silicate rocks, and skarns. We studied the Gustav orebody, which is located few hundred meters away from the contact with a large, late-orogenic Variscan Krkonoše–Jizera Plutonic Complex (KJPC) emplaced into shallow crust. Mineralogical and fluid inclusion study evidence indicates that the main sulfide stage, dominated by pyrrhotite, arsenopyrite, and chalcopyrite originated from aqueous hydrothermal fluids with salinity up to 8 wt% NaCl eq. with minimum homogenization temperatures ranging from 324 to 358 °C. These fluids mainly replaced carbonate-rich lithologies. Carbon, oxygen, and strontium isotope data in Ca-rich rocks imply total overprinting by channelized metasomatic fluid flow, which is most probably related to the intrusion of the KJPC, whereas δ³⁴S values of sulfides argue for a magmatic source of sulfur. The Re–Os age of arsenopyrite overlaps published age data for the KJPC and suggests synchronous formation of the main sulfide mineralization and pluton emplacement.
Trvalý link: http://hdl.handle.net/11104/0283996