Gela Gobejishvili’s research while affiliated with University of Georgia and other places

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Publications (1)


Figure 1. Dispersal of Sb-rich alloys and Sb metallic objects during the Chalcolithic period, Early Bronze Age (EBA), Middle Bronze Age (MBA), Late Bronze Age (LBA) and Early Iron Age (EIA).
Figure 2. Plan of the mine showing sampling points 1-3, which, respectively are samples Georgia 2, 3 and 4 (after Maisuradze and Gobejishvili 2001 ).
Figure 4. Isotopic composition of "China 3" (ore) during different digestion steps in experiment 2.
Figure 5. Isotopic composition of the final digestion phase of Procedure 1 and Procedure 3 for the ore samples "China 3" and "Georgia 6."
Figure 7. Sb isotopic data of Georgian stibnites and Sb-rich jewellery.

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Antimony as a raw material in ancient metal and glass making: provenancing Georgian LBA metallic Sb by isotope analysis
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November 2019

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29 Citations

STAR Science & Technology of Archaeological Research

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Peter Leeming

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Sb was frequently used as a raw material, both in ancient glass-making (as an opacifier and decolouriser) and metallurgy (either as an alloying element or as a pure metal). Despite this ubiquity, antimony production has only occasionally been studied and questions concerning its provenance are still not satisfactorily answered. This study evaluates the suitability of Sb isotope analysis for provenance determination purposes, as experiments under lab conditions have revealed fractionation occurring during redox processes in oxidising stibnites and in making opacified glasses. The results of this paper help to evaluate the possible influence of the pyrotechnological processes on the antimony isotope composition of glass artefacts. This paper focuses on the Caucasus as case study by applying mineralogical, geochemical and isotopic analysis to Georgian ores (mainly from the Racha-Lechkumi district) and Late Bronze Age (LBA; 15th–10th century BCE) metallic Sb objects found at the sites of Brili and Chalpiragorebi.

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... [7][8][9][10][11][12][13] Signicant Sb isotope fractionation can occur through chemical weathering, soil biogeochemical processes, redox reactions, adsorption, evaporation, and condensation processes, 7,14-26 although the fractionation factors are not yet entirely determined. Sb isotopes have been widely used in archaeology to trace the origin of Sb, 8,27 and they can also efficiently trace pollution sources and biogeochemical processes in hydrologic systems. 9,28,29 Additionally, Sb isotopes were used to identify redox changes in epithermal systems and ngerprint hydrothermal uid ow in high-temperature systems, 10,11 implying that Sb isotopes have great potential for tracing metal sources, ore-forming processes, uid evolution, and mineralization. ...

Reference:

Applying standard addition to determine antimony isotopes in low-Sb samples using HG-MC-ICP-MS
Antimony as a raw material in ancient metal and glass making: provenancing Georgian LBA metallic Sb by isotope analysis

STAR Science & Technology of Archaeological Research