Stibnite vein from Dębowina near Bardo (Polish Sudetes)

• Autorzy: Kotula P.

Identyfikatory

DOI

10.2478/ctg-2014-0004

• Języki publikacji: EN

Abstrakty

EN

In the contact zone of the Bardo Structure and Kłodzko-Złoty Stok Intrusion and Kłodzko Metamorphic, metasomatic orebearing quartz-carbonate veins rich in Sb, Zn, Cu, Ag, Au, Pb are present. In 1771 the mine ,,Reiche Silber Gluck” within stibnite vein was founded in Dębowina near Bardo. Its entrance was discovered again in 2007. The stibnite vein is mainly build of stibnite and sphalerite and of quartz and dolomite rich in Mn. Stibnite crystallizes as columnar or forming radiate centres and aciculars. Its crystals reach size to 2 mm. Sphalerite appears as individual anhedral and polymineralic grained concentrations reaching size to 2,5 mm. Earlier pyrite and arsenopyrite crystallized – they occur locally in this deposit. There were found also in the deposit tetrahedrite rich in Ag, what wasn't reported earlier in studies from the mine in Dębowina.

Słowa kluczowe

EN

Bardo Structure; stibnite; Agdeposit; old mines; propylitic; SEM

PL

Dębowina; Sudety; kopalnia; SEM

• Wydawca: De Gruyter
• Czasopismo: Contemporary Trends in Geoscience
• Rocznik: 2013
• Tom: Vol. 2, iss. 1
• Strony: 28--33
• Opis fizyczny: Bibliogr. 13 poz., wykr., tab., zdj.

Twórcy

autor

Kotula P.

• Faculty of Earth Science, University of Silesia, Bedzinska Str. 60, 41-200 Sosnowiec

Bibliografia

• 1. T.Dziekoński (1972), Wydobywanie i metalurgia kruszcow na Dolnym Śląsku od XIII do połowy XIX wieku, Wyd. PAN, Wrocław.(in Polish)
• 2. L.Grancea, L. Bailly, J. Leroy D. Banks, E. Marcoux, J. P. Mile, M. Cuney, A. S. Andre, D. I.C.Fabre (2002), Fluid evolution in the Baia Mare epithermal gold /polymetallic district, Inner Carpathians, Romania, Mineralium Deposita 37: 630–647
• 3. R.E. Krupp (1988), Solubility of stibnite in hydrogen sulphide solutions, speciation, and equilibrium constants, from 25 to 350 °C. Geochim Cosmochim Acta 52: 3005-3015
• 4. R. Kryza, J. Muszer, J. Haydukiewicz, C. August, M. Jurasik, N. Rodionov a A SIMS zircon age for a biostratigraphically dated Upper Visean (Asbian) bentonite in the Central-European Variscides (Bardo Unit, Polish Sudetes) g Int J Earth Sci (Geol Rundsch)100:1227–1235ner
• 5. J.Lis, H. Sylwestrzak (1986), Minerały Dolnego Śląska, Inst. Geol. Wyd. Geologiczne, Warszawa. (in Polish)
• 6. M. Mączka, M. Stysz (2008) Kopalnia ,,Reiche Silber Gluck: w Dębowinie – relikt dawnego gornictwa antymonu w Gorach Bardzkich. Dzieje gornictwa – element europejskiego dziedzictwa kultury, pod red. P.P. Zagożdzona i M. Madziarza, Wrocław (in Polish).
• 7. S. Mikulski (1998), Złotonośna mineralizacja kruszcowa z Barda Śląskiego (Sudety Środkowe). Przegląd Geologiczny 46(12); 1261-1267.
• 8. A.M.R. Neiva P. Andraš, J.M.F. Ramos (2008), Antimony quartz and antimony–gold quartz veins from northern Portugal, Ore Geology Reviews 34 533–546
• 9. W.E. Petrascheck (1933), Die Erzlagerstatten des Schlesischen Gebirges, Arch.Lagerst. Forsch. Heft 59.
• 10. R. H. Silitoe (2000), Gold-rich porphyry deposits: Descriptive and genetic models and their role in exploration and discovery. Review in Econimic Geology 13: 315-345.
• 11. H.P. Schwarcz, S.W. Burnie, (1973), Influence of sedimentary environments on sulfur isotope ratios in clastic rocks: A review. Mineralium Deposita 8:264-277
• 12. T.Wagner, N.J.Cook (1998), Sphalerite remobilization during multistage hydrothermal mineralization eventsexamples from siderite-Pb-Zn-Cu-Sb veins, Rheinisches Schiefergebirge, Germany, Mineralogy and Petrology 63:223-241.
• 13. T.Wagner, N.J.Cook (2000), Late-Variscan antimony mineralisation in the Rheinisches Schiefergebirge, NW Germany: evidence for stibnite precipitation by drastic cooling of high-temperature fluid systems, Mineralium Deposita 35: 206-222.

Uwagi

Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę.