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Article: Iron Isotopic Compositions of Geological Reference Materials and Chondrites

TitleIron Isotopic Compositions of Geological Reference Materials and Chondrites
Authors
KeywordsCalibration
Certified reference materials
Geological reference materials
Iron
Isotope ratios
Mass spectrometry
Precise determination
Issue Date2011
Citation
Geostandards and Geoanalytical Research, 2011, v. 35, n. 1, p. 101-123 How to Cite?
AbstractHigh-precision iron isotopic compositions for Fe-bearing geological reference materials and chondrites with a wide range of matrices (e.g., silicates, oxides, organic-bearing materials) are reported. This comprehensive data set should serve as a reference for iron isotopic studies across a range of geological and biological disciplines for both quality assurance and inter-laboratory calibration. Where comparison is available, the iron isotopic compositions of most geological reference materials measured in this study were in agreement with previously published data within quoted uncertainties. Recommendations for the reporting of future iron isotopic data and associated uncertainties are also presented. Long-term repeat analyses of all samples indicate that highly reproducible iron isotopic measurements are now obtainable (± 0.03‰ and ± 0.05‰ for δ56Fe and δ57Fe, respectively). © 2010 The Authors. Geostandards and Geoanalytical Research © 2010 International Association of Geoanalysts.
Persistent Identifierhttp://hdl.handle.net/10722/363138
ISSN
2023 Impact Factor: 2.7
2023 SCImago Journal Rankings: 0.922

 

DC FieldValueLanguage
dc.contributor.authorCraddock, Paul R.-
dc.contributor.authorDauphas, Nicolas-
dc.date.accessioned2025-10-10T07:44:47Z-
dc.date.available2025-10-10T07:44:47Z-
dc.date.issued2011-
dc.identifier.citationGeostandards and Geoanalytical Research, 2011, v. 35, n. 1, p. 101-123-
dc.identifier.issn1639-4488-
dc.identifier.urihttp://hdl.handle.net/10722/363138-
dc.description.abstractHigh-precision iron isotopic compositions for Fe-bearing geological reference materials and chondrites with a wide range of matrices (e.g., silicates, oxides, organic-bearing materials) are reported. This comprehensive data set should serve as a reference for iron isotopic studies across a range of geological and biological disciplines for both quality assurance and inter-laboratory calibration. Where comparison is available, the iron isotopic compositions of most geological reference materials measured in this study were in agreement with previously published data within quoted uncertainties. Recommendations for the reporting of future iron isotopic data and associated uncertainties are also presented. Long-term repeat analyses of all samples indicate that highly reproducible iron isotopic measurements are now obtainable (± 0.03‰ and ± 0.05‰ for δ<sup>56</sup>Fe and δ<sup>57</sup>Fe, respectively). © 2010 The Authors. Geostandards and Geoanalytical Research © 2010 International Association of Geoanalysts.-
dc.languageeng-
dc.relation.ispartofGeostandards and Geoanalytical Research-
dc.subjectCalibration-
dc.subjectCertified reference materials-
dc.subjectGeological reference materials-
dc.subjectIron-
dc.subjectIsotope ratios-
dc.subjectMass spectrometry-
dc.subjectPrecise determination-
dc.titleIron Isotopic Compositions of Geological Reference Materials and Chondrites-
dc.typeArticle-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1111/j.1751-908X.2010.00085.x-
dc.identifier.scopuseid_2-s2.0-79951938499-
dc.identifier.volume35-
dc.identifier.issue1-
dc.identifier.spage101-
dc.identifier.epage123-
dc.identifier.eissn1751-908X-

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