Publication:
GZ7 and GZ8 – Two Zircon Reference Materials for SIMS U-Pb Geochronology

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.date.issuedBE2561
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.format.mimetypeapplication/pdf
dc.identifier.citationGeostandards and Geoanalytical Research. Vol 42, No.4 (2018), p.431-457
dc.identifier.doi10.1111/ggr.12239
dc.identifier.issn16394488
dc.identifier.other2-s2.0-85054508859
dc.identifier.urihttps://hdl.handle.net/20.500.14740/5782
dc.rights.holderมหาวิทยาลัยศรีนครินทรวิโรฒ
dc.subject.otherBinary alloys
dc.subject.otherGeochronology
dc.subject.otherPlacers
dc.subject.otherSecondary ion mass spectrometry
dc.subject.otherSilicate minerals
dc.subject.otherTitanium alloys
dc.subject.otherUncertainty analysis
dc.subject.otherZircon
dc.subject.otherDecay constants
dc.subject.otherGeothermometry
dc.subject.otherMass fraction
dc.subject.otherPlacer deposits
dc.subject.otherReference material
dc.subject.otherStructure-related
dc.subject.otherU-Pb geochronology
dc.subject.otherWeighted mean
dc.subject.otherLead alloys
dc.titleGZ7 and GZ8 – Two Zircon Reference Materials for SIMS U-Pb Geochronology
dc.typeArticle
dspace.entity.typePublication
swu.datasource.scopushttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85054508859&doi=10.1111%2fggr.12239&partnerID=40&md5=5ca377b4d03c6c75b06a00efe26dea25

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