4.1 Article

MINERALOGY OF MEDIEVAL SLAGS FROM LEAD AND SILVER SMELTING (BOHUTIN, PRIBRAM DISTRICT, CZECH REPUBLIC): TOWARDS ESTIMATION OF HISTORICAL SMELTING CONDITIONS*

期刊

ARCHAEOMETRY
卷 51, 期 -, 页码 987-1007

出版社

WILEY
DOI: 10.1111/j.1475-4754.2008.00455.x

关键词

SLAGS; MEDIEVAL SMELTING; LEAD; SILVER; MINERALOGY; PRIBRAM DISTRICT; CZECH REPUBLIC

资金

  1. Charles University [GAUK 228/2006/B GEO]
  2. Ministry of Education, Youth and Sports of the Czech Republic [MSM 0021620855]

向作者/读者索取更多资源

Slags from the Pb/Ag medieval (14th century) smelting plant located at Bohutin, Pribram district, Czech Republic, were studied from the mineralogical and geochemical points of view. Two types of slags were distinguished: (i) quenched slags formed mainly by Pb-rich glass and unmelted residual grains of SiO2 and feldspars, and (ii) crystallized slags mainly composed of Fe-rich olivine (fayalite) and glass. The mean log viscosity value of the slags calculated for 1200 degrees C was 2.119 Pa s. The morphology of olivine crystals was used to estimate the cooling rates of the melt, for some slags indicating rates > 1450 degrees C/h. The projection of the bulk composition of slags onto the SiO2-PbO-FeO ternary system was used for rough temperature estimates of slag formation, lying probably between 800 and 1200 degrees C.

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