Abstract
Seven mineralogical-geochemical types of ores have been identified in the gold orogenic deposits of Uzbekistan: /Au-W/Au-Bi-Te/Au-As/Au-Ag-Te/Au-Ag-Se/Au-Sb/Au-Hg/. Non-industrial are Au-W and Au-Hg. For each industrial type, certain gold compounds are characteristic: maldonite, Au-arsenopyrite and Au-pyrite, petzite, physhesserite, petrovskaite, aurostibite, which form regular micro- nanoensembles with the corresponding minerals Bi, Te, Se, S, As, Sb. They are direct indicators of the type and technological properties of ores. Pyrite and arsenopyrite are preserved in the processing wastes of Au-Bi-Te and Au-As ores, in which gold (901‰), maldonite (Au2Bi), headleyite (Bi7Te3) and others were detected, 300–700 nm in size. Waste is suitable for the secondary extraction of gold.
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Koneev, R., Khalmatov, R., Tursunkulov, O., Krivosheeva, A., Iskandarov, N., & Sigida, A. (2019). Nanotechnologies in Mineral-Geochemical Methods for Assessing the Forms of Finding of Gold, Related Elements, Technological Properties of Industrial Ores and Their Tails. In Springer Proceedings in Earth and Environmental Sciences (pp. 99–102). Springer Nature. https://doi.org/10.1007/978-3-030-22974-0_22
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