Abstract
In this work, we studied the zoned olivine crystals from historical metallurgical slags by means of hyperspectral Raman mapping and Raman spectroscopy. As a result, we detected 3 crystal zones: central, intermediate and peripheral. The most important was the “gap” area within the intermediate zone with a Raman band typical for olivine. This defective area was formed due to quick melt crystallization and crystal absorption of glass microparticles and non-structural impurities.
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References
Ankushev MN, Artemyev DA, Blinov IA. Elementy-primesi v zonal’nyh olivinah metallurgicheskih shlakov bronzovogo veka na Yuzhnom Urale. Mineralogiya. 2018a;4(1):55-67. [Ankushev MN, Artemyev DA, Blinov IA. Trace elements in zoned olivines from the Bronze Age metallurgical slags at the Southern Urals. Mineralogy. 2018a;4(1):55–67 (In Russ.)].
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Acknowledgements
The study of the mineralogical features of historical metallurgical slags was supported by the Russian Science Foundation (Grant No. 16-18-10332). Raman spectroscopy was performed as a part of the topic No. AAAA-A18-118053090045-8 of the IGG UB RAS state assignment.
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Ankushev, M.N., Pankrushina, E.A., Blinov, I.A. (2020). Zoned Olivines in Metallurgical Slags of the Bronze Age: Electron Microscopy and Raman Mapping. In: Votyakov, S., Kiseleva, D., Grokhovsky, V., Shchapova, Y. (eds) Minerals: Structure, Properties, Methods of Investigation. Springer Proceedings in Earth and Environmental Sciences. Springer, Cham. https://doi.org/10.1007/978-3-030-49468-1_1
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