ID‐TIMS Sm‐Nd and Sr Isotope Ratios of Reference Material Basalt Ribeirão Preto (BRP‐1)

Author:

Neto Carla123ORCID,de Morisson Valeriano Claudio12ORCID,Enzweiler Jacinta4ORCID,Paravidini Gabriel23ORCID,Carvalho Manuela235ORCID,Heilbron Monica12ORCID,Lana Cristiano6ORCID,Larizzatti João Henrique7ORCID

Affiliation:

1. Laboratório de Geocronologia e Isótopos Radiogênicos, LAGIR Universidade do Estado do Rio de Janeiro Rua São Francisco Xavier 524 20550‐013 Rio de Janeiro RJ Brazil

2. Grupo de Pesquisa em Geotectônica, Tektos/UERJ Universidade do Estado do Rio de Janeiro Rua São Francisco Xavier 524 20550‐013 Rio de Janeiro RJ Brazil

3. Programa de Pós‐graduação em Geociências, PPGG/UERJ Universidade do Estado do Rio de Janeiro Rua São Francisco Xavier 524 20550‐013 Rio de Janeiro RJ Brazil

4. Universidade de Campinas, Unicamp, Rua Carlos Gomes 250 Cidade Universitária 13083‐855 Campinas SP Brazil

5. Fundação de Amparo à Pesquisa do Estado do Rio de Janeiro, FAPERJ Avenida Erasmo Braga 118 20020‐000 Rio de Janeiro RJ Brazil

6. Departamento de Geologia, Escola de Minas Universidade Federal de Ouro Preto, Campus Universitário Morro do Cruzeiro s/n 35400‐000 Ouro Preto MG Brazil

7. Serviço Geológico do Brasil, CPRM Avenida Pasteur 404 22290‐240 Rio de Janeiro RJ Brazil

Abstract

This work presents Sm‐Nd and Sr isotopic ratios of the BRP‐1 (“Basalt Ribeirão Preto”) reference material (RM) based on repeated TIMS measurements over twelve years carried out by the LAGIR laboratory, Brazil. The BRP‐1 RM was produced by the Brazilian Geological Survey from a ca. 130 Ma within‐plate basalt, collected from a quarry near Ribeirão Preto city in the Paraná basin. Isotope ratios were measured using a TRITON mass spectrometer. Instrumental bias and fractionation corrections were performed based on repeated measurements of the certified RMs JNdi‐1 and NIST SRM 987. The measured Nd and Sr isotopic ratios of BRP‐1 are: 143Nd/144Nd = 0.512408 ± 0.000010 (2s), and 87Sr/86Sr = 0.706011 ± 0.000017 (2s). The mass fractions of Sm and Nd are 11.0 ± 0.2 and 51.9 ± 0.6 μg g‐1, respectively, showing no significant differences compared with the accepted values from the literature. No significant difference between measurements was observed, whether digesting samples in single or batch mode, using metal‐jacketed PTFE bombs or PFA vials, or with or without the addition of a spike. The accuracy of these results was evaluated through the measurement of well‐characterised USGS RMs, such as AGV‐1, BCR‐1, BHVO‐1, G‐2 and GSP‐1.

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology,Geochemistry and Petrology,Geology

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