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Controlled Reduction of Iron Content in Zirconiun Ore:A Case Study in Polyphase Mineralization,Pocs de Caldas Alkaline Plateau

机译:锆矿中铁含量的可控减少:以Pocs de Caldas碱性高原多相矿化为例

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摘要

In PCAC(Po?os de Caldas Alkaline Complex),in southeastern Brazil,it is observed a polyphase mineralization related to Zr-,U-,Th-,Mo-,and REE-enrichment due to hydromethermal processes which affected alkaline primary rock.Primary Zr-minerals were leached and concentrated as“caldasite”,a rock composed mainly by zircon and baddeleyite in different proportions.Several techniques of mineralogical characterization were applied and results indicated zircon,baddeleyite,magnetite and iron-oxyhydroxides,mainly.Magnetic separation by WHIMS(Wet High-Intensity Magnetic Separation)was performed in order to indicate the efficiency for Fe-concentration removal for potential application in refractory industry.
机译:在巴西东南部的PCAC(Po?os de Caldas碱金属复合物)中,观察到由于热液热作用影响了碱性原生岩石,导致与Zr-,U-,Th-,Mo-和REE富集有关的多相矿化。初生的Zr矿物被沥滤并浓缩为“钙铁矿”,这是一种主要由不同比例的锆石和Baddeleyite组成的岩石。应用了多种矿物学表征技术,结果表明锆石,Baddeleyite,磁铁矿和羟基氧化铁主要成分。进行WHIMS(湿法高强度磁选)以表明去除铁精矿的效率,可用于耐火材料行业。

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