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首页> 外文期刊>Journal of the Geological Society of India >REE geochemistry of uranium-bearing columbite-tantalites and multiple oxide phases from proterozoic rare metal pegmatites of Pandikimal and adjoining areas, Jharsuguda district, Orissa
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REE geochemistry of uranium-bearing columbite-tantalites and multiple oxide phases from proterozoic rare metal pegmatites of Pandikimal and adjoining areas, Jharsuguda district, Orissa

机译:奥里萨邦贾尔苏格达地区潘迪基玛尔及其邻区的元古代稀有金属伟晶岩中含铀的钴钴矿-钽铁矿和多种氧化物相的稀土元素地球化学

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摘要

Rare earth element (REE) geochemistry of uranium bearing columbite-tantalite and multiple Nb-Ta oxide phases from the Pandikimal-Jangapara pegmatites, Jharsuguda district, Orissa have been studied and evaluated. Columbite-tantalite from these areas contain low Sigma REE (100-1000 ppm) with LREE/HREECN 0.5 and minor amounts of uranium (0.3-0.6%U3O8). Multiple oxide phases (yttrotantalite, samarskite, microlite and fergusonite) contain elevated amounts of U (10-11% U3O8) and REE (1.9-2.8%) with HREE>LREE. Plot of Sigma REE vs chondrite-normalised LREE/HREE shows positive correlation in 'U'rich multiple oxides compared to those from columbite-tantalites which tend to show a negative correlation. The LREE/HREE ratio is 0.24 with negative Eu anomaly (Eu/Eu* = 0.1) indicating evolved nature of these pegmatites.
机译:研究和评价了奥里萨邦贾里苏格达地区潘迪基马尔—贾加拉帕格伟晶岩中含铀的co钴-钽铁矿和多个Nb-Ta氧化物相的稀土元素(REE)地球化学。来自这些地区的哥伦比-钽铁矿含有低Sigma REE(100-1000 ppm)和LREE / HREECN 0.5,还有少量铀(0.3-0.6%U3O8)。多种氧化物相(钇钽铁矿,sa铁矿,微晶石和洋红铁矿)含有较高含量的U(10-11%U3O8)和REE(1.9-2.8%),且HREE> LREE。 Sigma REE与球粒陨石归一化LREE / HREE的关系图显示,与富含钴矿的钽铁矿相比,富'U'的多种氧化物呈正相关,而钴铁矿-钽铁矿往往呈负相关。 LREE / HREE比为0.24,负Eu异常(Eu / Eu * = 0.1)表明这些伟晶岩的演化性质。

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