Forms of occurrence and micro-nano ensambles of gold as indicators of formation conditions, spatial distribution, and type of orogenic deposits in Uzbekistan (South Tien Shan)

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Abstract

Gold ore deposits of Uzbekistan are confined to the South Tien Shan orogenic belt. They are located in black shales (Muruntau, Amantaytau, Daugyztau), terrigenous sedimentary (Kokpatas), volcanic (Balpantau), and intrusive (Zarmitan, Guzhumsai) rocks. Their age is 280—290 Ma and coincides with the age of post-collision granitoid magmatism. The deposits form Kyzylkum and Nurata mining districts. Gold forms micro-nanoparticles and is incorporated into diversified compounds with Bi, Sb, As, Te, Se, S, Ag, Hg in primary quartz-sulfide and sulfide ores. Seven mineral and geochemical types of ores are recognized: Au—W with scheelite and molybdenite; Au—Bi—Te with maldonite, tellurides, bismuth sulpho-tellurides; Au—As with pyrite, arsenopyrite, Ni—Co minerals; Au—Ag—Te with calaverite, petzite, hessite, etc.; Au—Ag—Se with fichesserite, acanthite, freibergite, agvilarite, petrovskite, etc.; Au—Sb—Ag with aurostibite, boulangerite, burnonite, cincenite, chalcostibite, tetrahedrite, etc.; Au—Hg with cinnabar, consbergite, Hg-bearing native gold. Recoverable resources are determined by 2—3 types of ores. Three main types of gold deposits are proposed on the base of outlined mineralogical and geochemical types: Au—W—Bi—Te (Muruntau, Myutenbay, Zarmitan); Au—As—Sb—Ag (Amantaytau, Kokpatas, Daugyztau); Au—Ag—Sb—Se (Kosmanachi, Okzhetpes). The emphasis on the nanomineral approach in the study of gold, its compounds, and micro-nano ensembles increases the efficiency of searching, typifying and evaluating the prospects of hidden mineralization, and is favorable to determine the conditions of formation and technological properties of gold ores.

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About the authors

Rustam I. Koneev

National University of Uzbekistan

Author for correspondence.
Email: ri.koneev@gmail.com

Doctor of Geological and Mineralogical Sciences, Professor of the Department Mineralogy and Geochemistry

Uzbekistan, Tashkent, Talabalar shaharchsi 1 

Rustam A. Khalmatov

Center for Advaced Technologies

Email: r.khalmatov@yahoo.com

Candidate of Geological and Mineralogical Sciences, Deputy Director for Science

Uzbekistan, Tashkent, Talabalar shaharchsi 3а

Anna N. Krivosheeva

National University of Uzbekistan

Email: 91k.anna@gmail.com

Master, PhD student, Department of Mineralogy and Geochemistry

Uzbekistan, Tashkent c., Talabalar shaharchsi 1 

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Supplementary files

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2. Fig. 1. Geological scheme of gold deposit locations in geodynamic structures of the Central Asia (Goldfarb et al., 2014).

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3. Fig. 2. Micro-nanomineral forms of gold and its compounds in different types of ores: I — Au—Bi—Te; II — Au—As; III — Au—Ag—Se; IV — Au—Sb.

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4. Fig. 3. Combined histogram of gold content for orogenic deposits in the Kyzylkum-Nurata region. N = 203.

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