High-alumina rocks from the Panimba and Mayakon areas (Yenisei Ridge): Composition and industrial perspectives

A. V. Nekipelova, E. Sokol, S. Kokh, I. Likhanov, P. Khvorov
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Abstract

Research subject. Аndalusite- and kyanite-bearing (13–19 wt % Al2SiO5) rocks of the Teya metamorphic complex (Mayakon and Panimba areas), Yenisei Ridge.Aim. To study the composition and mineral content of high-alumina rocks from the Panimba and Mayakon areas.Materials and methods. Laboratory mineral processing was employed to estimate the mineral content of metamorphic rocks of the Teya complex using a magnetic and gravity separation at the Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences (Novosibirsk). The concentrates were obtained from typical samples of andalusite, kyanite, and andalusite-kyanite metapilites. After crushing and grinding, the rock samples were separated into size fractions <0.06, 0.06 ≤ x < 0.1 and 0.1 ≤ x < 0.25 mm. The concentrates were recovered from size fractions ≥0.06 mm. Phase, bulk rock, and trace element composition of the rock samples, mineral concentrates, and other fractions were analyzed using XRD, XRF, ICP-MS, and SEM.Results. The magnetic product obtained at the first stage of mineral processing using magnetic separation accumalated staurolite, biotite, chlorite, ilmenite, pyrrhotite, and pyrite. At the second stage, light products containing quartz, feldspars, and muscovite were separated from non-magnetic products with CHBr3 using a centrifugal concentrator. At the last stage, using a double-knife separator, the heavy product from the previous beneficiation stage was separated into a “magnetic” raw concentrate (52–92 wt % Al2SiO5) and a “non-magnetic” final (70–97 wt % Al2SiO5) concentrate. The andalusite-kyanite concentrates (up to 97 wt % Al2SiO5) were obtained by the combination of cheapest and simplest methods of magnetic and gravity separation. The concentrates containing andalusite and kyanite with low recovery (0.7–6%) are comparable to the grade of kyanite-bearing ores of Karelia, the Kola Peninsula, and Gansu Province, China.Conclusions. The study shows that high-quality andalusite and/or kyanite concentrates can be recovered from high-alumina metapelites of the Teya metamorphic complex.
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Panimba和Mayakon地区(叶尼塞岭)的高铝岩:成分和工业前景
研究课题。Yenisei山脊Teya变质杂岩(Mayakon和Panimba地区)中含蓝晶石(13-19 wt % Al2SiO5)的Аndalusite岩石。研究了Panimba和Mayakon地区高铝岩的组成和矿物含量。材料和方法。在俄罗斯科学院西伯利亚分院地质与矿物学研究所(Novosibirsk),利用磁选和重力分离法,利用实验室矿物加工技术估计了Teya杂岩变质岩的矿物含量。从红柱石、蓝晶石和红柱石-蓝晶石的典型样品中获得精矿。破碎磨矿后,将岩样分离成小于0.06、0.06≤x < 0.1和0.1≤x < 0.25 mm的粒径段。精矿的回收粒度≥0.06 mm。采用XRD、XRF、ICP-MS、sem等分析了岩石样品、矿物精矿和其他组分的物相、整体岩石和微量元素组成。磁选选矿第一阶段获得的磁性产物主要为橄榄石、黑云母、绿泥石、钛铁矿、磁黄铁矿和黄铁矿。在第二阶段,含石英、长石和白云母的轻产物用CHBr3从非磁性产物中分离出来。在最后阶段,使用双刀分离机,将前一选矿阶段的重产品分离成“磁性”原精矿(52-92 wt % Al2SiO5)和“非磁性”终精矿(70-97 wt % Al2SiO5)。采用最便宜、最简单的磁选和重选相结合的方法,获得了红柱石-蓝晶石精矿(Al2SiO5质量分数高达97%)。含红柱石和蓝晶石的精矿回收率较低(0.7-6%),与中国甘肃省卡累利阿、科拉半岛和甘肃含蓝晶石矿石的品位相当。研究表明,从特雅变质杂岩的高铝变质岩中可回收出高质量的红柱石和蓝晶石精矿。
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