The Canadian Mineralogist; October 2007; v. 45; no. 5;
p. 1189-1200; DOI: 10.2113/gscanmin.45.5.1189
© 2007 Mineralogical Association of Canada
PRIMARY PHASES IN PYROMETALLURGICAL SLAGS FROM A ZINC-SMELTING WASTE DUMP,
WI
TOCH
OWICE, UPPER SILESIA, POLAND
Jacek Puziewicz1,
,
Katarzyna Zainoun2 and
Hubert Bril3
1 Instytut Nauk Geologicznych, Uniwersytet Wroc
awski, ul. Cybulskiego 30, 50–205 Wroc
aw, Polska
2 Instytut Nauk Geologicznych, Uniwersytet Wroc
awski, ul. Cybulskiego 30, 50–205 Wroc
aw, Polska and Équipe "Metallic Trace Elements", U.M.R. 6532 CNRS, HydrASA, Université de Limoges, 123, avenue Albert Thomas, F–87060 Limoges Cedex, France
3 Équipe "Metallic Trace Elements", U.M.R. 6532 CNRS, HydrASA, Université de Limoges, 123, avenue Albert Thomas, F–87060 Limoges Cedex, France

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FIG. 2. The material forming the dump. (a) The surface of the dump, formed of slag fragments of various size. (b) Huge fragment of slag with white accumulations of authigenic phases (indicated by the arrows). (c) Small (several cm in diameter) fragments of slag with a vesicular margin and a massive center. (d) Scoriaceous material with fragments of crucible.
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FIG. 3. Textures of slags from the wi toch owice waste dump. a) Granular texture of phase assemblage 1, consisting of red spinel embedded in matrix consisting of anhedral melilite, zincite and willemite. Optical image. (b) The same as (a), BSE image. (c) Texture of phase assemblage 4, with euhedral prisms of pyroxene embedded in melilite matrix. Optical image. (d) Phase assemblage 3, consisting of plagioclase, olivine, pyroxene and hyalophane. BSE image. Symbols used: znc: zincite, sp: spinel, wil: willemite, mel: melilite, ol: olivine, pl: plagioclase, px: pyroxene, hy: hyalophane.
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Copyright © 2008 by Mineralogical Association of Canada