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. 2017 Apr 17;375(2094):20150394. doi: 10.1098/rsta.2015.0394

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© 2017 The Authors.

Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, provided the original author and source are credited.

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Figure 1. — Mineral assemblages and relative abundances assumed to solidify from a terrestrial magma ocean. Trace elements and volatiles are not shown but would be incorporated into each phase in varying quantities. Adapted from figure 1 in Elkins-Tanton [20].