Analysis of the relative decay constants of 235U and 238U by multi-step CA-TIMS measurements of closed-system natural zircon samples
By J. Mattinson. 2010
268 citations recorded by the source corpus.
Subfields: Geophysics, Inorganic Chemistry
View Paper: https://www.semanticscholar.org/paper/09503a2d828b0de9f5e4d4bb29207ad9c23ac47b
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In Geophysics
- Pieter Vermeesch
- S. Bowring
- N. McLean
- James Frederick Bowring
- M. Horstwood
- A. Schmitt
- U. Schaltegger
- B. Schoene
In Inorganic Chemistry
- Pieter Vermeesch
- S. Bowring
- M. Horstwood
- A. Schmitt
- U. Schaltegger
- N. McLean
- James Frederick Bowring
- D. Condon
Citations in the corpus
- Evaluating uncertainties in the calibration of isotopic reference materials and multi-element isotopic tracers (EARTHTIME Tracer Calibration Part II) (2015, methodology): “…U and 238 U decay constant data (Jaffey et al., 1971) legitimizes further efforts at inter-calibrating the U decay constants (e.g. Schoene et al., 2006; Mattinson, 2010; Cheng et al., 2013) as well as the U–Pb system with other radio-isotopic dating systems through the analyses of assumed coeval…”
- An algorithm for U‐Pb isotope dilution data reduction and uncertainty propagation (2011, methodology): “…tracer and decay constants also contains elements for any covariance between the two, whichwould be incurred if for instance the 235U decay constant were recalibated to the 238U decay constant using closed system zircon analyses spiked with the same tracer [Schoene et al., 2006;Mattinson, 2010].”
- Community‐Derived Standards for LA‐ICP‐MS U‐(Th‐)Pb Geochronology – Uncertainty Propagation, Age Interpretation and Data Reporting (2016, background): “The cause of this discordance sits outside of the scope of this discussion, but at least in part stems from inaccuracy in k235U relative to k238U (Schoene et al. 2006, Mattinson 2010).”
- U–Th–Pb zircon geochronology by ID-TIMS, SIMS, and laser ablation ICP-MS: Recipes, interpretations, and opportunities (2015, background): “2 241 Additional factors to take into account are the values for the natural 238 U/ 235 U ratio in dated 242 materials (Condon et al., 2010; Hiess et al., 2012) and of uranium decay constants (Schoene 243 et al., 2006; Mattinson, 2010; Boehnke and Harrison, 2014).”