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Long-term repeatability and interlaboratory reproducibility of high-precision ID-TIMS U–Pb geochronology

Age determination of minerals using the U–Pb technique is widely used to quantify time in Earth's history. A number of geochronology laboratories produce the highest precision U–Pb dates employing the EARTHTIME (202)Pb–(205)Pb–(233)U–(235)U tracer solution for isotope dilution, and the EARTHTIM...

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Detalles Bibliográficos
Autores principales: Schaltegger, Urs, Ovtcharova, Maria, Gaynor, Sean P., Schoene, Blair, Wotzlaw, Jörn-Frederik, Davies, Joshua F. H. L., Farina, Federico, Greber, Nicolas David, Szymanowski, Dawid, Chelle-Michou, Cyril
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society of Chemistry 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8262554/
https://www.ncbi.nlm.nih.gov/pubmed/34276120
http://dx.doi.org/10.1039/d1ja00116g

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