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Mineralogical characterization and geochemical behavior of rare earth elements from a carbonatite deposit

机译:碳酸盐矿沉积物稀土元素的矿物学特征及地球化学行为

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The paper will focus on the geochemical characterization of the Montviel carbonatite deposit, located in Quebec (Canada). The five main lithologies of the deposit (ore and waste rocks) were sampled, characterized, and submitted to kinetic testing in order to investigate their REE leaching potential. A REE concentrate was also prepared from the ore sample using a combination of gravimetric and magnetic methods. All samples were submitted to a Qemscan analysis coupled to EPMA (electron probe microanalysis). These results indicate that the main REE bearing minerals are burbankite, Kukharenkoite-Ce, monazite, and apatite.The geochemical behavior of the waste rocks and ore samples was studied using humidity cells while a weathering cell (small-scale humidity cell) was used for the REE concentrate. The kinetic testing results show that low concentrations of light REE are leached (8.8-139.6 μ.g/1 total light REE) from the materials. These results are explained by a low reactivity of the REE bearing carbonates in the kinetic testing conditions, and by precipitation of secondary REE minerals.
机译:本文将专注于位于魁北克(加拿大)的蒙特维尔碳酸盐矿矿床的地球化学特征。沉积物(矿石和废岩)的五个主要岩性被取样,其特征,并提交给动力学测试,以调查其REE浸出潜力。还使用重量测定和磁性方法的组合从矿石样品制备REE浓缩物。将所有样品提交给偶联至EPMA(电子探针微分析)的qemscan分析。这些结果表明,主要的颈部矿物质矿物质是伯班德,Kukharenkoite-Ce,monazite和磷灰石。使用湿度细胞(小规模湿度细胞)使用湿度细胞进行废岩和矿石样品的地球化学行为。雷浓缩。动力学测试结果表明,低浓度的轻度射精来自材料的浸出(8.8-139.6μg/ 1总光圈)。这些结果是通过在动力学测试条件下的REE的低反应性解释,并通过仲胶质矿物的沉淀来解释。

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