B
Blair Schoene
Researcher at Princeton University
Publications - 118
Citations - 11770
Blair Schoene is an academic researcher from Princeton University. The author has contributed to research in topics: Zircon & Geochronology. The author has an hindex of 43, co-authored 101 publications receiving 9291 citations. Previous affiliations of Blair Schoene include Massachusetts Institute of Technology & University of Geneva.
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Plesovice zircon : A new natural reference material for U-Pb and Hf isotopic microanalysis
Jirri Slama,Jirri Slama,Jirri Slama,Jan Košler,Daniel J. Condon,James L. Crowley,Axel Gerdes,John M. Hanchar,Matthew S.A. Horstwood,George A. Morris,Lutz Nasdala,Nicholas Norberg,Urs Schaltegger,Blair Schoene,Michael Tubrett,Martin J. Whitehouse +15 more
TL;DR: The Plesovice zircon as discussed by the authors has a concordant U-Pb age with a weighted mean Pb-206/U-238 date of 337.13 +/- 0.37 Ma (ID-TIMS, 95% confidence limits, including tracer calibration uncertainty).
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Community‐Derived Standards for LA‐ICP‐MS U‐(Th‐)Pb Geochronology – Uncertainty Propagation, Age Interpretation and Data Reporting
Matthew S.A. Horstwood,Jan Košler,George E. Gehrels,Simon E. Jackson,Noah McLean,Chad Paton,Norman J. Pearson,Keith N. Sircombe,Paul J. Sylvester,Pieter Vermeesch,James F. Bowring,Daniel J. Condon,Blair Schoene +12 more
TL;DR: The LA-ICP-MS U-(Th-)Pb geochronology international community has defined new standards for the determination of U-(th)-Pb ages as discussed by the authors.
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Derivation of isotope ratios, errors, and error correlations for U‐Pb geochronology using 205Pb‐235U‐(233U)‐spiked isotope dilution thermal ionization mass spectrometric data
TL;DR: In this article, a comprehensive treatment of the derivation of U-Pb isotope ratios and their corresponding uncertainties from isotope dilution thermal ionization mass spectrometric measurements is presented.
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Reassessing the uranium decay constants for geochronology using ID-TIMS U–Pb data
TL;DR: In this paper, the U-Pb systematics of zircon and xenotime on the single-to sub-grain scale by high-precision ID-TIMS geochronology on 11 rock samples ranging from 0.1 to 3.3 Ga.
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Correlating the end-Triassic mass extinction and flood basalt volcanism at the 100 ka level
TL;DR: In this paper, high-precision U/Pb geochronology from volcanic ashes was used to show that the Triassic-Juras-sic boundary and end-Triassic biological crisis from two independent marine stratigraphic sections correlate with the onset of terrestrial fl ood volcanism in the Central Atlantic Magmatic Province to <150 ka.