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Access status: Open Access ,
Hydrothermal ore mineralization from the Polish part of the Tatra Mts., Central Western Carpathians
(Wydawnictwa AGH, 2021) Sitarz, Magdalena; Gołębiowska, Bożena; Nejbert, Krzysztof; Dimitrova, Dimitrina; Milovský, Ratislav
Several areas with hydrothermal ore mineralization are present in the Polish part of the Western Tatra Mts. Massive and disseminated sulfides, mainly minerals from the tetrahedrite group and chalcopyrite, fill quartz veins accompanied by siderite, dolomite and baryte - many of these were mined between the 16$^{th}$ and 18$^{th}$ century. This paper presents information on the mineralogy of the common sulfides and the preliminary studies of both the isotopic composition of sulfur in tetrahedrite as well as the origin of hydrothermal fluids. The most common primary sulfide minerals in the ores are tetrahedrite-(Zn) and tetrahedrite-(Fe) corresponding to Zn ranges from 1.83 to 5.87 wt.% (0.47–1.44 apfu), and Fe from 1.63 to 5.05 wt.% (0.48–1.52 apfu). The substitution of As for Sb shows maximum As content of 7.25 wt.% (1.588 apfu) which corresponds to the Sb/(Sb+As) = 0.60. Both varieties show substitutions of Bi and Hg, up 0.6 wt.% (0.049 apfu) and 0.96 wt.% (0.081 apfu), respectively, and content of trace elements: Co (max. 976 ppm), Cd (max. 735 ppm), In (max. 14 ppm). Chalcopyrite, pyrite, and galena show compositions close to the ideal formula. Differences in the content of trace elements in the studied tetrahedrite and chalcopyrite were explained by element partitioning between these minerals. The distributions of In, Ga and Sn in the studied minerals indicate that the mineralization was formed at low temperature and pressure. The homogenization temperature of the primary inclusions in quartz in the range of 120–174°C indicate the origin of mineralization in low temperature stage from low salinity fluids (up to 17.92 wt.% NaCl eq.). Stable $\delta^{34}S$ isotopes in minerals of the tetrahedrite group suggest that the igneous fluids might be one of the sources from which ores were crystallized.
Access status: Open Access ,
Primary and secondary copper minerals from Rędziny, Rudawy Janowickie, Sudeten, Southwestern Poland
(Wydawnictwa AGH, 2012) Orligóra, Wojciech; Gołębiowska, Bożena
Dolomite quarry in Rędziny is a place, which has a very rich polymetallic mineralization. It is a result of hydrothermal processes (precipitated primary minerals) or chemical weathering changes (precipitated secondary minerals). Proximity to Karkonosze Granite massif greatly influenced the variety of the mineralization in Rędziny. Compared to numerous exploited mines located in the vicinity (for example Miedzianka, Ciechanowice, Czarnów, Radomierz), the dolostone quarry is relatively young, opencast mine. Sulfides are the most common primary minerals in Rędziny. This information appears in the study of Gołębiowska et al. (e.g. 1998, 2006, 2012).
Access status: Open Access ,
Graftonite-sarcopside intergrowths in phosphate nodulas from pegmatite at Michałkowa, Sowie Mountains Block, SW Poland
(Wydawnictwa AGH, 2012) Grochowina, Anna; Gołębiowska, Bożena; Pieczka, Adam
Sareopside (Fe,Mn,Mg)$_{3}$(PO$_{4}$)$_{2}$ and graftonite (Fe,Mn,Ca)$_{3}$(PO$_{4}$)$_{2}$ are the dominant minerals found in the phosphate nodules from the Michałkowa pegmatite in the Sowie Mountains block.
Access status: Open Access ,
Manganese oxides from Zalas, Kraków area, southern Poland
(Wydawnictwa AGH, 2016) Polak, Marta; Gołębiowska, Bożena; Rzepa, Grzegorz
The Zalas quarry is located in the southern, marginal part of the Silesian-Cracovian Monocline.

Gołębiowska, Bożena

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