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. Author manuscript; available in PMC: 2019 Oct 1.
Published in final edited form as: Earth Planet Sci Lett. 2018 Aug 7;499:257–265. doi: 10.1016/j.epsl.2018.07.030

Figure 5:

Figure 5:

Effects of the timing of the Moon-forming impact, fraction of metal that equilibrates k, and equilibrating silicate mass on the resulting Earth 182W anomaly. a) Effects of varying k for a fixed equilibrating silicate mass (whole mantle equilibration). b) Effects of varying the equilibrating silicate mass for a fixed fraction of equilibrating metal (k = 0.55). Entire impactor silicate is always equilibrated; amount of target silicate equilibrating is varied. Symbol size is proportional to planetary mass. Open (filled) symbols indicate Earth analogues whose late veneer mass is greater (less) than 0.02 M. Each column of symbols represents one simulation, with the different colored symbols within the column representing different model conditions. Shaded region is Earth value.