期刊
SCIENCE
卷 335, 期 6076, 页码 1610-1614出版社
AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/science.1215507
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资金
- UK Natural Environment Research Council (NERC) [NE/C517909/1, IP/1028/0508]
- European Community [215458]
- NSF [EAR 0451802]
- Natural Environment Research Council [NE/C517909/1] Funding Source: researchfish
The present-day U-238/U-235 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 U-238/U-235 measurements for a suite of uranium-bearing minerals from 58 samples representing a diverse range of lithologies. This data set exhibits a range in U-238/U-235 values of >5 per mil, with no clear relation to any petrogenetic, secular, or regional trends. Variation between comagmatic minerals suggests that U-238/U-235 fractionation processes operate at magmatic temperatures. A mean U-238/U-235 value of 137.818 +/- 0.045 (2 sigma) 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 U-238/U-235 composition.
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