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GZ7 and GZ8 – Two Zircon Reference Materials for SIMS U‐Pb Geochronology

Here, we document a detailed characterisation of two zircon gemstones, GZ7 and GZ8. Both stones had the same mass at 19.2 carats (3.84 g) each; both came from placer deposits in the Ratnapura district, Sri Lanka. The U‐Pb data are in both cases concordant within the uncertainties of decay constants...

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Detalles Bibliográficos
Autores principales: Nasdala, Lutz, Corfu, Fernando, Schoene, Blair, Tapster, Simon R., Wall, Corey J., Schmitz, Mark D., Ovtcharova, Maria, Schaltegger, Urs, Kennedy, Allen K., Kronz, Andreas, Reiners, Peter W., Yang, Yue‐Heng, Wu, Fu‐Yuan, Gain, Sarah E. M., Griffin, William L., Szymanowski, Dawid, Chanmuang N., Chutimun, Ende, Martin, Valley, John W., Spicuzza, Michael J., Wanthanachaisaeng, Bhuwadol, Giester, Gerald
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6334521/
https://www.ncbi.nlm.nih.gov/pubmed/30686958
http://dx.doi.org/10.1111/ggr.12239
Descripción
Sumario:Here, we document a detailed characterisation of two zircon gemstones, GZ7 and GZ8. Both stones had the same mass at 19.2 carats (3.84 g) each; both came from placer deposits in the Ratnapura district, Sri Lanka. The U‐Pb data are in both cases concordant within the uncertainties of decay constants and yield weighted mean (206)Pb/(238)U ages (95% confidence uncertainty) of 530.26 Ma ± 0.05 Ma (GZ7) and 543.92 Ma ± 0.06 Ma (GZ8). Neither GZ7 nor GZ8 have been subjected to any gem enhancement by heating. Structure‐related parameters correspond well with the calculated alpha doses of 1.48 × 10(18) g(−1) (GZ7) and 2.53 × 10(18) g(−1) (GZ8), respectively, and the (U‐Th)/He ages of 438 Ma ± 3 Ma (2s) for GZ7 and 426 Ma ± 9 Ma (2s) for GZ8 are typical of unheated zircon from Sri Lanka. The mean U mass fractions are 680 μg g(−1) (GZ7) and 1305 μg g(−1) (GZ8). The two zircon samples are proposed as reference materials for SIMS (secondary ion mass spectrometry) U‐Pb geochronology. In addition, GZ7 (Ti mass fractions 25.08 μg g(−1) ± 0.18 μg g(−1); 95% confidence uncertainty) may prove useful as reference material for Ti‐in‐zircon temperature estimates.