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dc.date.accessioned2020-01-20T20:25:02Z
dc.date.available2020-01-20T20:25:02Z
dc.date.created2019-01-17T21:33:21Z
dc.date.issued2018
dc.identifier.citationNasdala, L Corfu, Fernando Schoene, B. Tapster, S.R. Wall, C.J. Schmitz, M.D. Ovtcharova, M. Schaltegger, U. Kennedy, A.K. Kronz, A. Reiners, P.W. Yang, Y.-H. Wu, F.-Y. Gain, S.E.M. Griffin, W.L. Szymanowski, D. Chanmuang, C. Ende, M. Valley, J.W. Spicuzza, M.J. Wanthanachaisaeng, B. Giester, G. . GZ7 and GZ8 – Two zircon reference materials for SIMS U-Pb geochronology. Geostandards and Geoanalytical Research. 2018, 42, 431-457
dc.identifier.urihttp://hdl.handle.net/10852/72342
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.
dc.languageEN
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleGZ7 and GZ8 – Two zircon reference materials for SIMS U-Pb geochronology
dc.typeJournal article
dc.creator.authorNasdala, L
dc.creator.authorCorfu, Fernando
dc.creator.authorSchoene, B.
dc.creator.authorTapster, S.R.
dc.creator.authorWall, C.J.
dc.creator.authorSchmitz, M.D.
dc.creator.authorOvtcharova, M.
dc.creator.authorSchaltegger, U.
dc.creator.authorKennedy, A.K.
dc.creator.authorKronz, A.
dc.creator.authorReiners, P.W.
dc.creator.authorYang, Y.-H.
dc.creator.authorWu, F.-Y.
dc.creator.authorGain, S.E.M.
dc.creator.authorGriffin, W.L.
dc.creator.authorSzymanowski, D.
dc.creator.authorChanmuang, C.
dc.creator.authorEnde, M.
dc.creator.authorValley, J.W.
dc.creator.authorSpicuzza, M.J.
dc.creator.authorWanthanachaisaeng, B.
dc.creator.authorGiester, G.
cristin.unitcode185,15,22,50
cristin.unitnameSeksjon for geologi og geofysikk
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.cristin1659798
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geostandards and Geoanalytical Research&rft.volume=42&rft.spage=431&rft.date=2018
dc.identifier.jtitleGeostandards and Geoanalytical Research
dc.identifier.volume42
dc.identifier.issue4
dc.identifier.startpage431
dc.identifier.endpage457
dc.identifier.doihttps://doi.org/10.1111/ggr.12239
dc.identifier.urnURN:NBN:no-75443
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn1639-4488
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/72342/2/Nasdala_et_al-2018-Geostandards_and_Geoanalytical_Research.pdf
dc.type.versionPublishedVersion
dc.relation.projectNFR/223272


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