Abstract
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 206Pb/ 238U 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 × 1018 g −1 (GZ7) and 2.53 × 1018 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.
Original language | English |
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Pages (from-to) | 431-457 |
Number of pages | 27 |
Journal | Geostandards and Geoanalytical Research |
Volume | 42 |
Issue number | 4 |
DOIs | |
Publication status | Published - Dec 2018 |
Bibliographical note
Copyright the Author(s) 2018. Version archived for private and non-commercial use with the permission of the author/s and according to publisher conditions. For further rights please contact the publisher.Keywords
- zircon
- reference material
- SIMS
- U-Pb geochronology
- Ti-in-zircon geothermometry
- NATURAL ZIRCON
- SINGLE ZIRCONS
- HF ISOTOPE MEASUREMENTS
- ENERGY-LEVELS
- TI-IN-ZIRCON
- MASS-SPECTROMETRY
- LU-HF
- RADIATION-DAMAGE
- HALF-LIVES
- HIGH-PRECISION