Mineralogy of precious metals in ores of the Yubileinoe porphyry gold deposit (Kazakhstan)

Author:

Plotinskaya O.Yu.1

Affiliation:

1. Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry RAS, Staromonenty per. 35, Moscow, 119017 Russia; plotin@igem.ru

Abstract

Gold and silver mineralogy is studied in ores of the Yubileinoe porphyry gold deposit (Kazakhstan). Native gold is the major gold mineral. Its fneness varies from 970‰ in magnetite-hematite assemblage to 733–860‰ in pyrite-chalcopyrite assemblage. Silver occurs as admixture in native gold and, occasionally, as silver telluride. Native gold is associated with bi and Pb minerals: rucklidgeite, galenaclaustalite, and tetradymite-kawazulite. According to chlorite geothermometry, the Au, Ag and bi minerals precipitated at temperatures of 250-230 °С. These features are typical of the porphyry gold deposits worldwide. Figures 5. Tables 3. References 17.

Publisher

South Urals Federal Research Center for Mineralogy and Geoecology of the Urals Branch of the RAS

Reference17 articles.

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3. [Annual report for 2015] (2015) AO AltynEx Company 43 p. https://kase.kz/fles/emitters/ATEC/atecp_2015_rus. pdf. Last accessed 01/05/2020. (in Russian).

4. Bailey S.W. (1988) Chlorites: structures and crystal chemistry. Hydrous Phyllosilicates (Exclusive of Micas). Reviews in Mineralogy, 19. washington, D.C., Mineralogical Society of America, 347–403.

5. Bespaev H.A., Globa V.A., Abishev V.M., Gulyaeva N.Ya. (1997) [Gold felds of Kazakhstan. Reference book]. Almaty, Informatcionno-analiticheskiy tsentr geologii, ekologii i prirodnyh resursov Respubliki Kazachstan. 144 p. (in Russian).

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