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European Journal of Mineralogy; August/September; v. 21; no. 4; p. 837-854; DOI: 10.1127/0935-1221/2009/0021-1942
© 2009 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Articles

Crystallization sequences in matte and speiss from primary lead metallurgy

Vojtech Ettler1,*, Zdenek Johan2, Petr Bezdicka3, Milan Drábek4 and Ondrej Sebek5

1 Institute of Geochemistry, Mineralogy and Mineral Resources, Charles University, Albertov 6, 128 43 Prague 2, Czech Republic
2 Bureau des Recherches Géologiques et Minières (BRGM), av. Claude Guillemin, 45060 Orléans Cedex 2, France
3 Institute of Inorganic Chemistry, Academy of Science of the Czech Republic, 250 68 Rez u Prahy, Czech Republic
4 Czech Geological Survey, Geologická 6, 152 00 Prague 5, Czech Republic
5 Laboratories of the Geological Institutes, Charles University, Albertov 6, 128 3 Prague 2, Czech Republic

* Corresponding author, e-mail: ettler{at}natur.cuni.cz

The temperature evolution and crystallization sequences in matte and speiss from Pb metallurgy at Príbram (Czech Republic) were determined using a combination of microscopic observations (optical microscopy, SEM/EDS), chemical microprobe data (EPMA), X-ray diffraction (XRD) of original samples collected at the dumps, and samples studied by heating experiments (temperature steps 25, 400, 700, 900, 1100, 1200 °C) and quenching experiments (400, 700 and 900 °C). Immiscibility of sulphide and metallic melts was observed. Identification of the major phases (sulphides, metals and intermetallic compounds) helped in estimation of the temperature of the matte and speiss solidification. Microscopic observations indicate that the crystallization sequences begin with high-temperature phases, such as Ni3Sn2 or NiSb (with melting temperatures of 1264 °C and 1147 °C, respectively) and, in sulphide melts, with crystallization of a high-temperature spinel phase (magnetite, Fe3O4), Fe-rich wurtzite/sphalerite (ZnS) and pyrrhotite (Fe1–xS). The solidification sequence ends either with the formation of galena + Cu sulphide eutectic (~500–600 °C) within the sulphide melt (matte), or with low-temperature Pb + Sb myrmekitic assemblage formation (247 °C) in the speiss. Possible geological implications related to the crystallization of sulphide ore bodies or their partial melting induced by regional metamorphic processes are discussed.

Key-words: matte, speiss, Pb metallurgy, sulphide melt, intermetallic melt, crystallization, solidification.







JOURNAL HOME HELP FEEDBACK/COMMNET SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers