Iron-loving elements are thought to have been added to Mars, Earth and the Moon after core formation. An analysis of meteorites formed in the first two to three million years of Solar System history suggests that a similar late veneer was added elsewhere too.
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References
Kimura, K., Lewis, R. S. & Anders, E. Geochim. Cosmochim. Acta 38, 683–701 (1974).
Day, J. M. D. et al. Nature Geosci. 5, 614–617 (2012).
Binzel, R. P. & Xu, S. Science 260, 186–191 (1993).
Kleine, T. et al. Geochim. Cosmochim. Acta 73, 5150–5188 (2009).
Ertel, W. et al. Geochim. Cosmochim. Acta 63, 2439–2449 (1999).
Borisov, A., Palme, H. & Spettel, B. Geochim. Cosmochim. Acta. 58, 705–716 (1994).
Dale, C. W. et al. Science 336, 72–75 (2012).
Shearer, C. K., Burger, P. & Papike, J. J. Geochim. Cosmochim. Acta 74, 4865–4880 (2010).
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Brenan, J. Ubiquitous late veneer. Nature Geosci 5, 591–592 (2012). https://doi.org/10.1038/ngeo1551
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DOI: https://doi.org/10.1038/ngeo1551