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Zircon M127 – A Homogeneous Reference Material for SIMS U–Pb Geochronology Combined with Hafnium,Oxygen and,Potentially, Lithium Isotope Analysis
Authors:Lutz Nasdala  Fernando Corfu  John W Valley  Michael J Spicuzza  Fu‐Yuan Wu  Qiu‐Li Li  Yue‐Heng Yang  Chris Fisher  Carsten Münker  Allen K Kennedy  Peter W Reiners  Andreas Kronz  Michael Wiedenbeck  Richard Wirth  Chutimun Chanmuang  Manuela Zeug  Tamás Váczi  Nicholas Norberg  Tobias Häger  Alfred Kröner  Wolfgang Hofmeister
Institution:1. Institut für Mineralogie und Kristallographie, Universit?t Wien, Wien, Austria;2. Department of Geosciences, University of Oslo, Oslo, Norway;3. Department of Geoscience, University of Wisconsin, Madison, WI, USA;4. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China;5. School of the Environment, Washington State University, Pullman, WA, USA;6. Institut für Geologie und Mineralogie, Universit?t zu K?ln, K?ln, Germany;7. Department of Imaging and Applied Physics, Curtin University of Technology, Bentley, Australia;8. Department of Geosciences, University of Arizona, Tucson, AZ, USA;9. Geowissenschaftliches Zentrum, Georg‐August‐Universit?t G?ttingen, G?ttingen, Germany;10. Helmholtz‐Zentrum Potsdam, Deutsches GeoForschungsZentrum, Potsdam, Germany;11. Faculty of Gems, Burapha University, Chanthaburi, Thailand;12. Institut für Geowissenschaften, Johannes Gutenberg‐Universit?t, Mainz, Germany;13. Beijing SHRIMP Center, Chinese Academy of Geological Sciences, Beijing, China
Abstract:In this article, we document a detailed analytical characterisation of zircon M127, a homogeneous 12.7 carat gemstone from Ratnapura, Sri Lanka. Zircon M127 has TIMS‐determined mean U–Pb radiogenic isotopic ratios of 0.084743 ± 0.000027 for 206Pb/238U and 0.67676 ± 0.00023 for 207Pb/235U (weighted means, 2s uncertainties). Its 206Pb/238U age of 524.36 ± 0.16 Ma (95% confidence uncertainty) is concordant within the uncertainties of decay constants. The δ18O value (determined by laser fluorination) is 8.26 ± 0.06‰ VSMOW (2s), and the mean 176Hf/177Hf ratio (determined by solution ICP‐MS) is 0.282396 ± 0.000004 (2s). The SIMS‐determined δ7Li value is ?0.6 ± 0.9‰ (2s), with a mean mass fraction of 1.0 ± 0.1 μg g?1 Li (2s). Zircon M127 contains ~ 923 μg g?1 U. The moderate degree of radiation damage corresponds well with the time‐integrated self‐irradiation dose of 1.82 × 1018 alpha events per gram. This observation, and the (U–Th)/He age of 426 ± 7 Ma (2s), which is typical of unheated Sri Lankan zircon, enable us to exclude any thermal treatment. Zircon M127 is proposed as a reference material for the determination of zircon U–Pb ages by means of SIMS in combination with hafnium and stable isotope (oxygen and potentially also lithium) determination.
Keywords:zircon  reference material     SIMS     U–  Pb geochronology  oxygen isotopes  hafnium isotopes  lithium   isotopes  Zircon  maté  riau de ré    rence     SIMS       ochronologie U‐Pb  isotopes d'oxygè  ne  isotopes du hafnium  isotopes du lithium
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