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. Author manuscript; available in PMC: 2019 May 1.
Published in final edited form as: Icarus. 2019 Jan 21;323:1–15. doi: 10.1016/j.icarus.2019.01.012

Figure 12.

Figure 12.

Mg and Si isotopic shifts with evaporation of CI-like planetesimals vs. fractions of Mg and Si remaining in the melt, respectively. The composition of Earth as represented by BSE relative to a CI chondrite starting material is shown for comparison (circle with cross).