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. Author manuscript; available in PMC: 2019 Apr 24.
Published in final edited form as: Meteorit Planet Sci. 2015 Apr 24;50(5):976–1004. doi: 10.1111/maps.12445

Figure 21.

Figure 21.

Predicted composition of olivine by MELTS. The Fe content increases monotonically as the temperature decreases. The Mn content also increases essentially monotonically, but is almost constant below 1300 °C. The Ca content increases to a maximum at 940 °C and then decreases again at lower temperatures.