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EPMA, micro-PIXE, synchrotron microprobe and TEM study of visible and invisible accumulations of Au and PGE in black shale and organic matrix, Kupferschiefer, Poland

Published online by Cambridge University Press:  05 July 2018

H. Kucha ,
W. Przyblowicz ,
M. Lankosz ,
F. Van Langevelde  and
K. Traxel
H. Kucha
Affiliation:
Institute of Geology and Mineral Deposits, 30-059 Krakow, Avenue Mickiewicza 30, Poland
W. Przyblowicz
Affiliation:
Institute of Physics and Nuclear Techniques, 30-059 Krakow, Avenue Mickiewicza 30, Poland
M. Lankosz
Affiliation:
Institute of Physics and Nuclear Techniques, 30-059 Krakow, Avenue Mickiewicza 30, Poland
F. Van Langevelde
Affiliation:
Department of Physics and Astronomy, Free University, 1081 HV, Amsterdam, The Netherlands
K. Traxel
Affiliation:
Physikalisches Institut der Unviersität Heidelberg, D-6900 Heidelberg 1, Germany
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Abstract

The Kupferschiefcr contains from 0.3 to 30 wt.% of organic matter, with an average value close to 10 wt.%. The concentration of heavy metals increases strongly towards the base of a black shale horizon. Where the black shale rests directly on red sandstone, the bottom few mm of the shale may contain (ppm): Hg 8-1500, mean 174; Ag 310-5780, mean 1222; Au 1-3000, mean 40; Pd 2-1000, mean 37; Pt 2-340, mean 18. The shale, enriched in noble metals, is overlain by thucholite shale. The flotation sulphide concentrate contains 1-3 ppm Au and a detectable Pd and Pt content. Selected gravity concentrates from the black shale contain 4-56 ppm Au, up to 25 ppm Pd, while the Pt content does not exceed 1 ppm. A tightly intermixed clay-organic matrix of the noble metal-bearing shale contains small accumulations of Au, Pt and Pd presumably as organomctallic compounds.

Thucholite is present locally. It contains inclusions of uraninite, brannerite and noble metal minerals lcoated at the boundary between optically isotropic and anisotropic components. The optically homogeneous organic matrix of the thucholite contains discrete inclusions of UO2, brannerite, electrum and organic compounds of Au, U, Pt and Ni varying in size from 0.008 to 0.025 μm as shown by TEM. Gold occurs in a continuous Au-Ag series. Refractory Au is present as substitutions in native silver and in the organic matrix of the shale and thucholite. Palladium forms several arsenides and sulphoarsenides. Refractory Pd is present as substitutions in Ni-Co arsenides and in the organic matrix of the shale and thucholite. Platinum is present as substitutions in the organic matrix of the noblemetal- bearing shale and thucholite.

The average detection limits of micro-PIXE were 8-10 ppm, and those of the SXRFA from one to a few ppm. A major factor defining detection limits in the studied samples were minor uranium lines overlapping spectral lines of the studied elements.

Keywords

noble metalsorganometallic compoundsthucholiteKupferschieferLubinPoland
Type
Petrology and Geochemistry
Information
Mineralogical Magazine , Volume 57 , Issue 386 , March 1993 , pp. 103 - 112
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1993

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References

Banas, M., Jarosz, J., and Salamon, W. (1978) Mineral. Pol., 9, 3–21.Google Scholar
Campbell, J. L., and Coockson, J. A. (1984) Nucl. Instr. and Meth., B3, 185-97.Google Scholar
Campbell, J. L., Perujo, A., Teesdale, W. J., and Coockson, J. A. (1988) Ibid. B30, 317-23.Google Scholar
Currie, L. A. (1968) Anal. Chem., 40, 586–593.Google Scholar
Kajfosz, J. (1987) lnt. Rep. of the Lab. of Applied Nuclear Spectroscopy. Institute of Nuclear Physics, Krakov, Poland (in Polish).Google Scholar
Kajfosz, J. and Kwiatek, W. M. (1987) Nucl. Instr. and Meth., B22, 78-81.Google Scholar
Kopp, O. C., Reeves, D. K., Rivers, M. L., and Smith, J. V. (1990) Chem. Geol., 81, 337–47.Google Scholar
Kucha, H. (1975) Mineral. Pol., 6, 87–92.Google Scholar
Kucha, H. (1976) Ann. Soc. Geol. Pol., 46, 369–417.Google Scholar
Kucha, H. (1981) Tschermak's Min. Petr. Mitt., 28, 1–16.Google Scholar
Kucha, H. (1982) Econ. Geol., 77, 1578–91.Google Scholar
Kucha, H. (1983) Trans. lnstn Min. Metall., 92, B72-B79.Google Scholar
Kucha, H. (1984) Chemie Erde, 43, 27–43.Google Scholar
Kucha, H. (1985) Trans. Instn Min. Metall., 94, B133-46.Google Scholar
Kucha, H. (1990) Geologische Rundschau, 79, 387–99.Google Scholar
Kucha, H. Mayer, W., and Piestrzynski, A. (1983) Mineral. Pol., 14, 35–43.Google Scholar
Kucha, H. and Wieczorek, A. (1988) Mineral. Deposita, 23, 174–8.Google Scholar
Piestrzynski, A. (1990) Ibid., 25, 146-51.Google Scholar
Przybylowicz, W., Kucha, H., Kajfosz, J. and Szymczyk, S. (1989) Proc. 12th Int. Conf. on X-ray Optics and Microanalysis, Krakov, Poland (Ed. S. Jasienska), 929 pp.Google Scholar
Przybylowicz, W., Kucha, H., Kajfosz, J. and Szymczyk, S. H., Pietrzynski, A., Traxel, K., and Bajt, S. (1990) Nucl. Instr. and Meth., B50, 231-7.Google Scholar
Przybylowicz, W. Langevelde Van, F., Kucha, H., Lankosz, M., and Wyszomirski, P. (1992) Nucl. Instr. and Meth., B68, 115-21.Google Scholar
Remond, G., Cesbron, F., Traxel, K., Campbell, J. L., and Cabri, L. J. (1987) Scanning Microscopy, 1, 1017–23.Google Scholar
Salamon, W. (1979) Mineral. Trans. Acad. Pol. Sei., 62, 59 pp. (in Polish).Google Scholar
Sawlowicz, Z. (1985) Mineral. Pol., 16, 35–42.Google Scholar
Ziebold, T. (1967) Anal. Chem., 39, 858–61.Google Scholar