Conference paper

Zircon M257 -: a homogeneous natural reference material for the ion microprobe U-Pb analysis of zircon


Authors listNasdala, Lutz; Hofmeister, Wolfgang; Norberg, Nicholas; Mattinson, James M.; Corfu, Fernando; Doerr, Wolfgang; Kamo, Sandra L.; Kennedy, Allen K.; Kronz, Andreas; Reiners, Peter W.; Frei, Dirk; Kosler, Jan; Wan, Yusheng; Goetze, Jens; Haeger, Tobias; Kroener, Alfred; Valley, John W.

Publication year2008

Pages247-265

JournalGeostandards and Geoanalytical Research

Volume number32

Issue number3

ISSN1639-4488

eISSN1751-908X

DOI Linkhttps://doi.org/10.1111/j.1751-908X.2008.00914.x

Conference17th Annual V M Goldschmidt Conference

PublisherWiley


Abstract
We introduce and propose zircon M257 as a future reference material for the determination of zircon U-Pb ages by means of secondary ion mass spectrometry. This light brownish, flawless, cut gemstone specimen from Sri Lanka weighed 5.14 g (25.7 carats). Zircon M257 has TIMS-determined, mean isotopic ratios (2s uncertainties) of 0.09100 +/- 0.00003 for (206)pb/U-238 and 0.7392 +/- 0.0003 for (207)pb/U-235. Its (206)pb/U-238 age is 561.3 +/- 0.3 Ma (unweighted mean, uncertainty quoted at the 95% confidence level); the U-Pb system is concordant within uncertainty of decay constants. Zircon M257 contains similar to 840 mu g g(-1) U (Th/U similar to 0.27). The material exhibits remarkably low heterogeneity, with a virtual absence of any internal textures even in cathodoluminescence images. The uniform, moderate degree of radiation damage (estimated from the expansion of unit-cell parameters, broadening of Raman spectral parameters and density) corresponds well, within the "Sri Lankan trends", with actinide concentrations, U-Pb age, and the calculated alpha fluence of 1.66 x 10(18) g(-1). This, and a (U+Th)/He age of 419 +/- 9 Ma (2s), enables us to exclude any unusual thermal history or heat treatment, which could potentially have affected the retention of radiogenic Pb. The oxygen isotope ratio of this zircon is 13.9%o VSMOW suggesting a metamorphic genesis in a marble or calc-silicate skarn.



Citation Styles

Harvard Citation styleNasdala, L., Hofmeister, W., Norberg, N., Mattinson, J., Corfu, F., Doerr, W., et al. (2008) Zircon M257 -: a homogeneous natural reference material for the ion microprobe U-Pb analysis of zircon, Geostandards and Geoanalytical Research, 32(3), pp. 247-265. https://doi.org/10.1111/j.1751-908X.2008.00914.x

APA Citation styleNasdala, L., Hofmeister, W., Norberg, N., Mattinson, J., Corfu, F., Doerr, W., Kamo, S., Kennedy, A., Kronz, A., Reiners, P., Frei, D., Kosler, J., Wan, Y., Goetze, J., Haeger, T., Kroener, A., & Valley, J. (2008). Zircon M257 -: a homogeneous natural reference material for the ion microprobe U-Pb analysis of zircon. Geostandards and Geoanalytical Research. 32(3), 247-265. https://doi.org/10.1111/j.1751-908X.2008.00914.x



Keywords


geochronologyGEOCHRONOLOGYID-TIMSM257MAGMATISMMETAMICTIZATIONOXYGEN-ISOTOPE RATIOSReference materialSecondary ion mass spectrometryshrimpTRACE-ELEMENTU-Pbzircon

Last updated on 2025-01-04 at 23:59