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Science. 2012 Mar 30;335(6076):1610-4. doi: 10.1126/science.1215507.

238U/235U Systematics in terrestrial uranium-bearing minerals.

Author information

1
NERC Isotope Geoscience Laboratory, British Geological Survey, Keyworth, Nottinghamshire, UK. jies@bgs.ac.uk

Abstract

The present-day (238)U/(235)U ratio has fundamental implications for uranium-lead geochronology and cosmochronology. A value of 137.88 has previously been considered invariant and has been used without uncertainty to calculate terrestrial mineral ages. We report high-precision (238)U/(235)U measurements for a suite of uranium-bearing minerals from 58 samples representing a diverse range of lithologies. This data set exhibits a range in (238)U/(235)U values of >5 per mil, with no clear relation to any petrogenetic, secular, or regional trends. Variation between comagmatic minerals suggests that (238)U/(235)U fractionation processes operate at magmatic temperatures. A mean (238)U/(235)U value of 137.818 ± 0.045 (2σ) in zircon samples reflects the average uranium isotopic composition and variability of terrestrial zircon. This distribution is broadly representative of the average crustal and "bulk Earth" (238)U/(235)U composition.

PMID:
22461608
DOI:
10.1126/science.1215507
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