Keppler and Golabek Graphite floatation on a magma

Keppler and Golabek Graphite floatation on a magma
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Keppler and Golabek Graphite floatation on a magma ocean and the fate of carbon during core formation Keppler and Golabek (2019) Geochem. Persp. Let. 11, 12-17 doi: 10.7185geochemlet.1918 2019 The Authors Published by the European

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Keppler and Golabek
Graphite floatation on a magma ocean and the fate of carbon during core formation Keppler and Golabek (2019) Geochem. Persp. Let. 11, 12-17 | doi: 10.7185/geochemlet.1918 © 2019 The Authors
Published by the European Association of Geochemistry
under Creative Commons License CC BY-NC-ND. Figure 4 The fate of carbon during core formation of a terrestrial planet. Maximum possible carbon content in the core as a function of the number of impact events by planetary embryos, for oxygen fugacities from IW-6 to IW-2 and a surface temperature of 2000 K (left scale); predicted maximum fraction of total carbon sequestered in the core (right scale) for a terrestrial planet with a bulk carbon content of 500 ppm (Marty, 2012).<br>