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DC Field | Value | Language |
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dc.contributor.author | Nasdala L. | |
dc.contributor.author | Corfu F. | |
dc.contributor.author | Schoene B. | |
dc.contributor.author | Tapster S.R. | |
dc.contributor.author | Wall C.J. | |
dc.contributor.author | Schmitz M.D. | |
dc.contributor.author | Ovtcharova M. | |
dc.contributor.author | Schaltegger U. | |
dc.contributor.author | Kennedy A.K. | |
dc.contributor.author | Kronz A. | |
dc.contributor.author | Reiners P.W. | |
dc.contributor.author | Yang Y.-H. | |
dc.contributor.author | Wu F.-Y. | |
dc.contributor.author | Gain S.E.M. | |
dc.contributor.author | Griffin W.L. | |
dc.contributor.author | Szymanowski D. | |
dc.contributor.author | Chanmuang N. C. | |
dc.contributor.author | Ende M. | |
dc.contributor.author | Valley J.W. | |
dc.contributor.author | Spicuzza M.J. | |
dc.contributor.author | Wanthanachaisaeng B. | |
dc.contributor.author | Giester G. | |
dc.date.accessioned | 2021-04-05T03:05:11Z | - |
dc.date.available | 2021-04-05T03:05:11Z | - |
dc.date.issued | 2018 | |
dc.identifier.issn | 16394488 | |
dc.identifier.other | 2-s2.0-85054508859 | |
dc.identifier.uri | https://ir.swu.ac.th/jspui/handle/123456789/12712 | - |
dc.identifier.uri | https://www.scopus.com/inward/record.uri?eid=2-s2.0-85054508859&doi=10.1111%2fggr.12239&partnerID=40&md5=5ca377b4d03c6c75b06a00efe26dea25 | |
dc.description.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. © 2018 The Authors. Geostandards and Geoanalytical Research published by John Wiley & Sons Ltd on behalf of International Association of Geoanalysts | |
dc.subject | Binary alloys | |
dc.subject | Geochronology | |
dc.subject | Placers | |
dc.subject | Secondary ion mass spectrometry | |
dc.subject | Silicate minerals | |
dc.subject | Titanium alloys | |
dc.subject | Uncertainty analysis | |
dc.subject | Zircon | |
dc.subject | Decay constants | |
dc.subject | Geothermometry | |
dc.subject | Mass fraction | |
dc.subject | Placer deposits | |
dc.subject | Reference material | |
dc.subject | Structure-related | |
dc.subject | U-Pb geochronology | |
dc.subject | Weighted mean | |
dc.subject | Lead alloys | |
dc.title | GZ7 and GZ8 – Two Zircon Reference Materials for SIMS U-Pb Geochronology | |
dc.type | Article | |
dc.rights.holder | Scopus | |
dc.identifier.bibliograpycitation | Geostandards and Geoanalytical Research. Vol 42, No.4 (2018), p.431-457 | |
dc.identifier.doi | 10.1111/ggr.12239 | |
Appears in Collections: | Scopus 1983-2021 |
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