A Mercury-like component of early Earth yields uranium in the core and high mantle 142Nd
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/nature14350.pdf
Reference31 articles.
1. Boyet, M. & Carlson, R. W. 142Nd evidence for early (>4.53 Ga) global differentiation of the silicate Earth. Science 309, 576–581 (2005).
2. Boyet, M. & Carlson, R. W. A new geochemical model for the Earth’s mantle inferred from (SM)-S-146-Nd-142 systematics. Earth Planet. Sci. Lett. 250, 254–268 (2006).
3. Campbell, I. H. & O’Neill, H. S. C. Evidence against a chondritic Earth. Nature 483, 553–558 (2012).
4. Wade, J. & Wood, B. J. The Earth’s ‘missing’ niobium may be in the core. Nature 409, 75–78 (2001).
5. Kinoshita, N. et al. A shorter Sm-146 half-life measured and implications for Sm-146-Nd-142 chronology in the Solar System. Science 335, 1614–1617 (2012).
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