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dc.contributor.authorNasdala L.
dc.contributor.authorCorfu F.
dc.contributor.authorSchoene B.
dc.contributor.authorTapster S.R.
dc.contributor.authorWall C.J.
dc.contributor.authorSchmitz M.D.
dc.contributor.authorOvtcharova M.
dc.contributor.authorSchaltegger U.
dc.contributor.authorKennedy A.K.
dc.contributor.authorKronz A.
dc.contributor.authorReiners P.W.
dc.contributor.authorYang Y.-H.
dc.contributor.authorWu F.-Y.
dc.contributor.authorGain S.E.M.
dc.contributor.authorGriffin W.L.
dc.contributor.authorSzymanowski D.
dc.contributor.authorChanmuang N. C.
dc.contributor.authorEnde M.
dc.contributor.authorValley J.W.
dc.contributor.authorSpicuzza M.J.
dc.contributor.authorWanthanachaisaeng B.
dc.contributor.authorGiester G.
dc.date.accessioned2021-04-05T03:05:11Z-
dc.date.available2021-04-05T03:05:11Z-
dc.date.issued2018
dc.identifier.issn16394488
dc.identifier.other2-s2.0-85054508859
dc.identifier.urihttps://ir.swu.ac.th/jspui/handle/123456789/12712-
dc.identifier.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85054508859&doi=10.1111%2fggr.12239&partnerID=40&md5=5ca377b4d03c6c75b06a00efe26dea25
dc.description.abstractHere, 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.subjectBinary alloys
dc.subjectGeochronology
dc.subjectPlacers
dc.subjectSecondary ion mass spectrometry
dc.subjectSilicate minerals
dc.subjectTitanium alloys
dc.subjectUncertainty analysis
dc.subjectZircon
dc.subjectDecay constants
dc.subjectGeothermometry
dc.subjectMass fraction
dc.subjectPlacer deposits
dc.subjectReference material
dc.subjectStructure-related
dc.subjectU-Pb geochronology
dc.subjectWeighted mean
dc.subjectLead alloys
dc.titleGZ7 and GZ8 – Two Zircon Reference Materials for SIMS U-Pb Geochronology
dc.typeArticle
dc.rights.holderScopus
dc.identifier.bibliograpycitationGeostandards and Geoanalytical Research. Vol 42, No.4 (2018), p.431-457
dc.identifier.doi10.1111/ggr.12239
Appears in Collections:Scopus 1983-2021

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