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Thiosulphates as precursors of banded sphalerite and pyrite at Bleiberg, Austria

Published online by Cambridge University Press:  05 July 2018

H. Kucha  and
E. F. Stumpfl
H. Kucha
Affiliation:
Institute of Geology and Mineral Deposits, 30-059 Krakow, Ave. Mickiewicza 30, Poland
E. F. Stumpfl
Affiliation:
Institute of Geological Sciences, Mining University, A-8700 Leoben, Austria
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Abstract

Banded sphalerite from Bleiberg, Austria, contains ubiquitous relics of Fe-thiosulphates and Fesulphites up to 50 μm in size. Zn, Pb, Ni and As form admixtures ranging from a few to 12 wt.% in these compounds. It is suggested that banded sphalerite is formed by a replacement of banded thiosulphate and thiosulphite precursors. This suggestion is supported by a significant admixture of Fe 0.41-8.20 wt.%) and the presence of goethite inclusions in banded sphalerite. In contrast, crystalline ZnS intergrown with the banded variety is Ni-free and contains only 0.06-0.14 wt.% Fe.

Banded pyrite contains inclusions of Fe-thiosulphate up to 200 μm in size. These thiosulphates contain (wt.%): 0.09-1.92 Zn, and 2.67−4.02 Pb. Pyrite formed by replacement (breakdown) of Fethiosulphate precursors contains 3.69-3.83 wt.% Pb.

It is suggested that banded sulphides precipitate from solutions carrying sulphur with mixed valances, and crystalline sulphides grow from solutions where the dominant dissolved sulphur is in the form of sulphidic anions.

Keywords

sphaleritepyritethiosulphatethiosulphitebandingBleibergAustria
Type
Petrology and Geochemistry
Information
Mineralogical Magazine , Volume 56 , Issue 383 , June 1992 , pp. 165 - 172
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1992

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References

Faesler, A. and Goehring, M. (1952) Rrntenspectrum und Bindungszustand die Ka Fluorescenstrahlung des Schwefels. Naturwiss., 39, 169–77.CrossRefGoogle Scholar
Greenwood, N. N. and Earnshaw, A. (1984) Chemistry of the Elements, Pergamon Press, Oxford, 1542 pp.Google Scholar
Jenkins, R. and de Vries, J. L. (1975) Practical X-ray spectrometry, 2nd edition, Springer, 189 pp.Google Scholar
Kneen, W. R., Roger, M. J. W., and Simpson, P. (1972) Chemistry, facts, patterns and principles. Addison-Wesley, 861 pp.Google Scholar
Kucha, H. (1988) Biogenic and non-biogenic concentration of sulfur and metals in the carbonate-hosted Ballinalock Zn-Pb deposit, Ireland. Mineralogy and Petrology, 38, 171–8.CrossRefGoogle Scholar
Kucha, H. (1990) Geochemistry of the Kupferschiefer, Poland. Geol. Rundschau, 79, 387–99.CrossRefGoogle Scholar
Kucha, H. Wouters, R., and Arkens, O. (1989) Determination of sulfur and iron valence by microprobe. Scanning Microscopy, 3, No. 1, 89–97.Google Scholar
Lehr, J. R., Seale, S. K., Wilhide, W. D., and Ash, D. H. (1980) Sulfide sulfur by X-ray fluorescence. Norelco Report, 527, No. 3, 10–12.Google Scholar
Mann, A. W. (1984) Mobility of gold and silver in lateritic weathering profiles: some observations from Western Australia. Econ. Geol., 79, 38–49.CrossRefGoogle Scholar
Paar, W. H., Braithwaite, R. S. W., Chen, T. T., and Keller, P. (1984) A new mineral, scotlandite (PbSO3) from Leadhills, Scotland: the first naturally occurring sulfite. Mineral Mag., 48, 283-8.CrossRefGoogle Scholar
Pryor, W. A. (1960) The kinetics of the disproportiona-tion of sodium thiosulphate to sodium sulphide and sulphate. Am. Chem. Soc. J., 82, 4794-7.CrossRefGoogle Scholar
Ramdohr, P. (1980) The ore minerals and their inter-growths. 2nd ed., Pergamon, I, 440 pp; 2, 1207 pp.Google Scholar
Stanton, R. L. (1989) The precursor principle and the possible significance of stratiform ores and related chemical sediments in the elucidation of processes of regional metamorphic mineral formation. Phil. Trans. Roy. Soc. Lond., A 328, 529452.Google Scholar
Valensi, G., Muylder Van, J., and Pourbaix, M. (1963) Soufre. In Atlas d'Equilibres Electrochimiques at 25°C (Pourbaix, M., Zoubov de, N., Muylder Van, J., eds.) Paris, Gauthier-Viullars, 644 pp.Google Scholar
Webster, J. G. (1987) Thiosulphate in surfieial geother-mal waters, North Island, New Zealand. Appl. Geochem., 2, 579-84.CrossRefGoogle Scholar