DEGEO - Departamento de Geologia

URI permanente desta comunidadehttp://www.hml.repositorio.ufop.br/handle/123456789/8

Navegar

Filtros

20201

Configurações

Autor: search.filters.author.Rodrigues, Daniel Aparecido da SilvaAssunto: search.filters.subject.Banded iron formations

Resultados da Pesquisa

Agora exibindo 1 - 1 de 1
  • Nenhuma Miniatura Disponível
    Item
    Determination of rare earth elements in Fe-minerals using external calibration by LA-ICP-MS and application on Cauê Iron Formation (Brazil).
    (2020) Sousa, Denise Versiane Monteiro de; Abreu, Adriana Trópia de; Sampaio, Geraldo Magela Santos; Lana, Cristiano de Carvalho; Rodrigues, Daniel Aparecido da Silva; Nalini Júnior, Hermínio Arias
    The rare earth elements (REE) composition in Fe-mineral phases is an important tool in iron formation studies to obtain information about parent rocks and environmental and paragenetic processes. However, the determination of REE presents some difficulties, such as the low concentration of these elements, matrix complexity and lack of iron matrix certified reference materials. The aim of the present work is to propose an analytical method to determine the REE plus Y (REE + Y) contents at trace levels in Fe-(hydr)oxides by the laser ablation ICPquadrupoleMS technique, using external calibration. The calibration curves were obtained from analyses of reference materials with different matrices, and the analytical conditions were checked on the NIST 614 glass. The linearity (R2 ≥ 0.98), limit of detection (0.002–0.044 μg g−1), limit of quantification (0.008–0.146 μg g−1), recovery (88.4–112.4%), and intraday (0.1–14.1%) and interday (1.6–17.8%) precision were systematically assessed. The results obtained showed that the method is fit for the purpose and showed evidence of a nonsignificant interference of the matrix. Thus, the developed procedure was applied in the analyses of magnetite, martite, hematite, and goethite grains from Cauê Iron Formation (Brazil). The REE + Y patterns of the minerals are consistent with the previous study of bulk analyses on whole rocks and highlight the postdepositional signature of these elements in banded iron formations.