Primitive Solar System materials and Earth share a common initial 142Nd abundance
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/nature19351.pdf
Reference44 articles.
1. Nyquist, L. E. et al. 146Sm-142Nd formation interval for the lunar mantle material. Geochim. Cosmochim. Acta 59, 2817–2837 (1995)
2. Boyet, M. & Carlson, R. W. 142Nd evidence for early (>4.53 Ga) global differentiation of the silicate Earth. Science 309, 576–581 (2005)
3. Carlson, R. W., Boyet, M. & Horan, M. Chondrite barium, neodymium, and samarium isotopic heterogeneity and early Earth differentiation. Science 316, 1175–1178 (2007)
4. Gannoun, A., Boyet, M., Rizo, H. & El Goresy, A. 146Sm–142Nd systematics measured in enstatite chondrites reveals a heterogeneous distribution of 142Nd in the solar nebula. Proc. Natl Acad. Sci. 108, 7693–7697 (2011)
5. Jellinek, A. M. & Jackson, M. G. Connections between the bulk composition, geodynamics and habitability of Earth. Nat. Geosci. 8, 587–593 (2015)
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