4.5 Article

Medieval Pb (Cu-Ag) Smelting in the Colline Metallifere District (Tuscany, Italy): Slag Heterogeneity as a Tracer of Ore Provenance and Technological Process

Journal

MINERALS
Volume 11, Issue 2, Pages -

Publisher

MDPI
DOI: 10.3390/min11020097

Keywords

slags; archaeometry; archaeology; medieval; lead; zinc; silver; smelting; Tuscany

Funding

  1. U-Med (Origins of a new economic union (7th-12th centuries): resources, landscapes and political strategies in a Mediterranean region)
  2. European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program [670792]
  3. European Research Council (ERC) [670792] Funding Source: European Research Council (ERC)

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Archaeological investigations in the Colline Metallifere district of Southern Tuscany, Italy, have revealed several Medieval sites near major Cu-Pb-Fe (Ag) ore deposits. This study focuses on late-medieval slags from Cugnano and Montieri, using geochemical and mineralogical methods to understand slag heterogeneities resulting from ore differences and technological processes. The distribution of matte-rich slags with different compositions can provide insights into the ore-gangue association and technological processes employed in the two sites.
Archaeological investigations of the Colline Metallifere district (Southern Tuscany, Italy) have highlighted several Medieval sites located close to the main Cu-Pb-Fe (Ag) ore occurrences. This study is focused on the investigation of late-medieval slags from Cugnano and Montieri sites using both geochemical and mineralogical methods to understand slag heterogeneities as result of ore differences and technological processes. Matte-rich slags present in both sites (with abundant matte +/- speiss and frequent relict phases) represent waste products related to primary sulphide ore smelting to obtain a raw lead bullion. The distribution of slags between the Ca-rich or Fe-rich dominant composition, and the consequent mineralogy, are tracers of the different ore-gangue association that occurred in the two sites. Silver is present only in very small matte-rich slags and ores enclosed within the mortar of the Montieri site; wastes derived from silver-rich mineral charges were probably crushed for the recovery of silver. Matte-poor slags found at Montieri represent a second smelting; raw lead bullion obtained from matte slags (both Fe- and Ca-rich) was probably re-smelted, adding silica and Al2O3-phase-rich fluxes, under more oxidizing conditions to reduce metal impurities. This second step was probably employed for Zn-rich lead ores; this process helped to segregate zinc within slags and improve the quality of the metal.

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