Mineral Forms of Tungsten at the Porokhovskoe and Yugo-Konevskoe Deposits (Southern Urals)

IF 0.8 4区 地球科学 Q3 GEOLOGY
D. A. Rogov, E. V. Belogub, K. A. Novoselov, M. A. Rassomakhin, R. R. Irmakov, A. E. Chugaev
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Abstract

Ore hand specimens and technological ore samples from the greisen-type Porokhovskoe and Yugo-Konevskoe tungsten deposits in the Southern Urals were studied. The major tungsten minerals in primary ores of both deposits are hübnerite and scheelite. Secondary and accessory minerals are pyrite, chalcopyrite and molybdenite; rare minerals are sphalerite, galena, bismuthinite, aikinite, unidentified Bi chalcogenides and sulfosalts, magnetite, rutile, ilmenite, titanite, and columbite. Veins are mainly composed by quartz–muscovite aggregate with secondary (calcite, dolomite, and fluorite), minor (chlorite and amphibole), and accessory (zircon, apatite, and uraninite). No distinct zonation in the distribution pattern of wolframite with varying Fe content relative to the Yugo-Konevsky granite pluton is identified. However, wolframites from the Northern area of the Porokhovskoe deposit are enriched in Fe compared to those from the Central area and Yugo-Konevskoe deposit. Along with through vein wolframite and scheelite, the oxidized ores also contain Fe and Mn oxyhydroxides, malachite, pyromorphite, and bromargyrite. Tungsten enters the composition of Mn and Fe oxyhydroxides, which replace wolframite and less often sulfides. The WO3 content in pseudomorphs of Mn and Fe oxyhydroxides after hübnerite reaches 18 wt %. Single grains of stolzite and russellite are found. According to the results of phase chemical analysis of technological samples, the amount of tungstite in oxidized ores is minor. Due to this, all ores of both deposits can be ascribed to primary technological type.

Abstract Image

波罗霍夫斯科和尤戈-科涅夫斯科矿床(南乌拉尔)的钨矿物形态
摘要研究了南乌拉尔地区绿森型Porokhovskoe和Yugo-Konevskoe钨矿床的手工标本和技术矿石样本。这两个矿床原生矿石中的主要钨矿物是白钨矿和白钨矿。次生和附属矿物为黄铁矿、黄铜矿和辉钼矿;稀有矿物为闪锌矿、方铅矿、铋矿、黝帘石、不明铋瑀和硫化物、磁铁矿、金红石、钛铁矿、榍石和铌铁矿。矿脉主要由石英-黑云母集合体组成,次生(方解石、白云石和萤石)、少量(绿泥石和闪石)和附属(锆石、磷灰石和铀矿石)。与 Yugo-Konevsky 花岗岩岩体相比,在不同铁含量的黑钨矿分布模式中没有发现明显的分带。不过,与中部地区和 Yugo-Konevskoe 矿床的黑钨矿相比,Porokhovskoe 矿床北部地区的黑钨矿富含铁。除了透脉黑钨矿和白钨矿,氧化矿石中还含有铁和锰氧氢氧化物、孔雀石、黄铁矿和溴钨矿。钨进入锰和铁氧氢氧化物的成分,取代黑钨矿和较少见的硫化物。在锰和铁氧氢氧化物的假象中,WO3 含量达到 18 wt %。此外,还发现了单粒的 stolzite 和 russellite。根据技术样本的相化学分析结果,氧化矿石中的钨矿量很少。因此,这两个矿床的所有矿石都可以归为原生技术类型。
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来源期刊
Geology of Ore Deposits
Geology of Ore Deposits 地学-地质学
CiteScore
1.10
自引率
14.30%
发文量
24
审稿时长
6-12 weeks
期刊介绍: Geology of Ore Deposits is a periodical covering the topic of metallic and nonmetallic mineral deposits, their formation conditions, and spatial and temporal distribution. The journal publishes original scientific articles and reviews on a wide range of problems in theoretical and applied geology. The journal focuses on the following problems: deep geological structure and geodynamic environment of ore formation; distribution pattern of metallogenic zones and mineral deposits; geology and formation environment of large and unique metallic and nonmetallic deposits; mineralogy of metallic and nonmetallic deposits; physicochemical and isotopic characteristics and geochemical environment of ore deposition; evolution of ore-forming systems; radiogeology and radioecology, economic problems in exploring, developing, and mining of ore commodities.
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