Non-chondritic iron isotope ratios in planetary mantles as a result of core formation
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://www.nature.com/articles/ngeo2896.pdf
Reference56 articles.
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4. Poitrasson, F., Halliday, A. N., Lee, D. C., Levasseur, S. & Teutsch, N. Iron isotope differences between Earth, Moon, Mars and Vesta as possible records of contrasted accretion mechanisms. Earth Planet. Sci. Lett. 223, 253–266 (2004).
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