Bismuth minerals from Yugo-Konevo and Porokhovskoe tungsten deposits (South Urals)
Author:
Kasatkin A.V.1, Belogub E.V.2, Kuznetsov A.M.3, Novoselov K.A.2, Skoda R.4, Nestola F.5, Rogov D.A.2
Affiliation:
1. Fersman Mineralogical Museum RAS, Moscow, Russia; anatoly.kasatkin@gmail.com 2. Institute of Mineralogy, South Urals Federal Research Center of Mineralogy and Geoecology UB RAS, Miass, Chelyabinsk Region, Russia 3. Chelyabinsk, Russia 4. Masaryk University, Brno, Czech Republic 5. University of Padova, Padova, Italy
Abstract
A mineral assemblage including sulfosalts of the bismuthinite-aikinite (aikinite, bismuthinite, gladite, salzburgite, krupkaite, lindstromite, pekoite, friedrichite, hammarite), pavonite (makovickyite, cupromakovickyite, pavonite, dantopaite, mummeite), cupropavonite (cupromakopavonite, cupropavonite) and lillianite (lillianite s.s.) homologous series, as well as angelaite, berryite, matildite, baksanite, ikunolite, tetradymite, hedleyite and native bismuth is identifed in veinlet ores of the Yugo-Konevo and Porokhovskoe tungsten deposits (Chelyabinsk oblast, South Urals). The Bi minerals occur as individual grains or intergrowths in fuorite-muscovite-quartz veins with hubnerite and scheelite , inclusions in quartz and intersticial aggregates between pyrite, sphalerite and galena. Angelaite, dantopaite, cupromakovickyite and cupromakopavonite are frst found at the territory of Russian Federation and salzburgite, cupropavonite, makovickyite and mummeite are found for the frst time in the South Urals.
Publisher
South Urals Federal Research Center for Mineralogy and Geoecology of the Urals Branch of the RAS
Subject
General Medicine,General Medicine,General Medicine,General Medicine,General Earth and Planetary Sciences,General Environmental Science,General Medicine,General Earth and Planetary Sciences,General Environmental Science,General Medicine,Industrial and Manufacturing Engineering,Materials Science (miscellaneous),Business and International Management,General Engineering
Reference32 articles.
1. Bonstedt-Kupletskaya E.M. (1943) [Mineralogy of the Karas’evskoe and Yugo-Konevskoe tungsten deposits in the Central Urals]. Doklady Akademii nauk SSSR [Doklady Academy of Sciences of the USSR], 40(9), 412–415. (in Russian) 2. Chvileva T.N., Bezsmertnaya M.S., Spiridonov E.M., Agroskin A.S., Papayan G.V., Vinogrado-va R.A., Lebedeva S.I., Zavyalov E.N., Filimonova A.A., Petrov V.K., Rautian L.P., Sveschnikova O.L. (1988) [Handbook of ore minerals in refected light]. Moscow, Nedra, 504 p. (in Russian) 3. Cook N.J., Ciobanu C.L. (2003) Lamellar minerals of the cuprobismutite series and related paderaite: a new occurrence and implications. The Canadian Mineralogist, 41, 441–456. 4. Ciobanu C.L., Cook N.J., Damian F., Damian G. (2006) Gold scavenged by bismuth melts: an example from alpine shear-remobilizates in the Highis Massif, Romania. Mineralogy and Petrology, 87, 351–384. 5. Damdinova L.B., Damdinov B.B., Huang X.W., Bryansky N.V., Khubanov V.B., Yudin D.S. (2019). Age, conditions of formation, and fuid composition of the Pervomaiskoe molybdenum deposit (Dzhidinskoe ore feld, South-Western Transbaikalia, Russia). Minerals, 9(10), 572.
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