Please use this identifier to cite or link to this item: http://www.repositorio.ufop.br/jspui/handle/123456789/10181
Title: The Diamantina monazite : a new Low‐Th reference material for microanalysis.
Authors: Gonçalves, Guilherme de Oliveira
Lana, Cristiano de Carvalho
Cipriano, Ricardo Augusto Scholz
Buick, Ian S.
Gerdes, Axel
Kamo, Sandra L.
Corfu, Fernando
Rubatto, Daniela
Wiedenbeck, Michael
Nalini Júnior, Hermínio Arias
Oliveira, Luiz Carlos Alves de
Keywords: U-Pb geochronology
Sm-Nd
Oxygen isotopes
Araçuaí orogen.
Issue Date: 2018
Citation: GONÇALVES, G. de O. et al. The Diamantina monazite : a new Low‐Th reference material for microanalysis. Geostandards And Geoanalytical Research, v. 22, n. 1, p. 25-47, 2018. Disponível em: <https://onlinelibrary.wiley.com/doi/abs/10.1111/ggr.12192>. Acesso em: 03 mai. 2018.
Abstract: Most monazite reference materials (RMs) for in situ U-Pb geochronology are rich in Th; however, many hydrothermal ore deposits contain monazite that is low in trace element contents, including Th, U and Pb. Because of potential problems with matrix effects and the lack of appropriate matrix-matched RMs, such variations can bias dating of hydrothermal deposits. In this paper, we describe a polycrystalline low-U and low-Th Diamantina monazite from the Espinhac o Range, SE Brazil. It has a U-Pb ID-TIMS weighted mean 207Pb*/235U ratio of 0.62913 ± 0.00079, 206Pb*/238U of 0.079861 ± 0.000088 and 207Pb*/206Pb* of 0.057130 ± 0.000031, yielding a weighted mean 206Pb*/238U date of 495.26 ± 0.54 Ma (95% c.l.). In situ dates acquired with different methods (LA-(Q, SF, MC)-ICP-MS and SIMS) are within uncertainty of the ID-TIMS data. U-Pb LA-(Q, MC)-ICP-MS runs, using Diamantina as a primary RM, reproduced the ages of other established RMs within < 1% deviation. The LA-MC-ICP-MS analyses yielded homogeneous Sm-Nd isotopic compositions (143Nd/144Nd = 0.511427 ± 23, 2s; 147Sm/144Nd = 0.1177 ± 13, 2s) and eNd(495 Ma) of -18.7 ± 0.5 (2s). SIMS oxygen isotope determinations showed measurement reproducibility better than ± 0.3‰ (2s), confirming Diamantina’s relative homogeneity at test portion masses below 1 ng.
URI: http://www.repositorio.ufop.br/handle/123456789/10181
metadata.dc.identifier.uri2: https://onlinelibrary.wiley.com/doi/abs/10.1111/ggr.12192
ISSN: 1751908X
Appears in Collections:DEGEO - Artigos publicados em periódicos

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