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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 2:

Figure 2:

Effect of partial equilibration of metal and silicate on the resulting mantle 182W anomaly. Each data point is the median of 73 Earth analogues, with error bars representing a 68% two-sided confidence interval. Shaded region indicates Earth value. Data labels are the depth of equilibration (expressed as a fraction of the evolving core-mantle boundary pressure) for the case of whole mantle equilibration. Data are slightly offset horizontally for clarity. Color indicates amount of equilibrating silicate: impactor silicate only (yellow), impactor+target silicate with a mass of 3× that of the impactor silicate (orange), and entire impactor+target silicate (red).