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Geochemical and mineralogical characteristics of calamines from the Olkusz zinc and lead ore district (South Poland)

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Abstrakty
EN
The mineralogical and geochemical characteristics of calamines developed from chemical weathering within two different tectonic settings (tectonic horst and graben) are described. Calamines collected from the Olkusz-Pomorzany and the Bolesław zinc and lead mines were analysed geochemically by means of EMP and SEM-EDS and their mineralogical composition was identified by using reflected light microscopy and XRD analysis. The calamines from the Olkusz-Pomorzany mine are composed of marcasite, galena, cerussite, sphalerite, hemimorphite, smithsonite and goethite. Hemimorphite prevails over smithsonite and occurs in the vicinity of primary sulphides. The mineralogical composition of the calamines from the Bolesław area is less diverse. These are primarily composed of goethite and smithsonite, with a minor content of marcasite and remnant sphalerite. The mineral composition of weathering sites in the Olkusz-Pomorzany and Bolesław areas may reflect different geochemical conditions (from slightly acidic to alkaline pH values, from lower to higher CO2 partial pressure and solutions of different silica saturation) that could have changed over time. The mineralogical compositions of the calamines differ quantitatively and this could reflect the tectonic setting of the primary ore affecting the rate of chemical weathering.
Rocznik
Strony
699--710
Opis fizyczny
Bibliogr. 43 poz., rys., tab., wykr.
Twórcy
  • Adam Mickiewicz University, Institute of Geology, Krygowskiego 12, 61-680 Poznań, Poland
  • Adam Mickiewicz University, Institute of Geology, Krygowskiego 12, 61-680 Poznań, Poland
Bibliografia
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  • 23. Lara, R.H., Briones, R., Monroy, M.G., Mullet, M., Humbert, B., Dossot, M., Naja, G.M., Roel, C., 2011. Galena weathering under simulated calcareous soil conditions. Science of the Total Environment, 409: 3971-3979.
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  • 27. McPhail, D.C., Summerhayes, E., Welch, S., Brugger, J., 2003.The geochemistry and mobility of zinc in the regolith. Advances in Regolith: 287-291.
  • 28. Nieć, M., Blajda, R., Niedzielski, B., 1993. Zinc-lead ore deposit in Lower Triassic (Roethian) dolomites at Bolesław (Olkusz region, Poland). Geological Quarterly, 37 (2): 157-174.
  • 29. Osman, AEM, 1989. Smithsonite in the oxidation zone of the Upper Silesia Zn-Pb ore deposits (Orzeł Biały mine, Bytom area) Poland. Mineralogia Polonica, 20: 57-65.
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  • 33. Sass-Gustkiewicz, M., Dżułyński, S., 1998. On the origin of strata-bound Zn-Pb ores in the Upper Silesia, Poland. Annales Societatis Geologorum Poloniae, 68: 267-278.
  • 34. Saas-Gustkiewicz, M., Dżułyński, S., Ridge, J. D., 1982. The emplacement of zinc-lead sulfide ores in the Upper-Silesian district-a contribution to the understanding of Mississippi Valley-Type deposits. Economic Geology, 77: 392-412.
  • 35. Strzelska-Smakowska, B., 2010. Nonsulfide zinc deposits in the Silesia-Kraków district (in Polish with English abstract). Biuletyn Państwowego Instytutu Geologicznego, 439: 371-374.
  • 36. Sutley, S., Sass-Gustkiewicz, M., Mayer, W., Leach, D., 1999. Mineralogy and chemistry of oxidized ores from the Upper Silesia Mississippi Valley-Type zinc-lead deposits, Poland. USGS Open File Report.
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  • 38. Szczerba, M., Sawłowicz, Z., 2009. Remarks on the origin of cerussite in the Upper Silesian Zn-Pb deposits, Poland. Mineralogia, 40: 53-64.
  • 39. Szuwarzyński, M., 1996. Ore bodies in the Silesian-Kraków Zn-Pb ore district, Poland. Prace Państwowego Instytutu Geologicznego, 154: 9-24.
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Uwagi
Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2020).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-f360d02e-9b3d-4829-9b28-0d559759659b
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