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Beneficiation of vanadium-bearing magnetite from the Sinarsuk Deposit, West Greenland

机译:来自西格陵兰山脉储存的钒磁铁矿的矿物

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Vanadium mineralization occurs in oxide-rich horizons within layered metagabbro zones of the Sinarsuk deposit, West Greenland. The main oxide minerals are vanadiferous magnetite and ilmenite, comprising 30% to ~90% of the rock volume and the ratio of magnetite to ilmenite ranges from ~3:2 to ~4:1. Magnetite and ilmenite have vanadium concentrations ranging from 1.93 to 2.68 wt.%, and 0.32 to 0.59 wt.%, respectively, equivalent V_2O_5. Preliminary beneficiation of two composite bulk samples shows the samples can be beneficiated fairly easily using low-intensity magnetic separation at a coarse grind (106 to 600 microns) to yield a vanadiferous magnetite concentrate.
机译:钒矿化发生在西格陵兰西部矿床的层状Metagrabbo区内的富含氧化物地平线中。主要的氧化物矿物是钒磁铁矿和Ilmenite,包含30%至〜90%的岩石体积和磁铁矿与Ilmenite的比例范围为约3:2至〜4:1。磁铁矿和Ilmenite的钒浓度为1.93-2.68重量%,分别为0.32至0.59重量%,分别为等效的V_2O_5。两种复合体样品的初步份额显示样品可以在粗磨(106至600微米)下使用低强度磁分离相当容易地受益,得到钒磁铁矿浓缩物。

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