Extended Data Fig. 8: Comparison of major element composition of Commondale parental melt with incremental melt model liquid at 5 GPa and 1,827 °C. | Nature

Extended Data Fig. 8: Comparison of major element composition of Commondale parental melt with incremental melt model liquid at 5 GPa and 1,827 °C.

From: Deep, ultra-hot-melting residues as cradles of mantle diamond

Extended Data Fig. 8

There is a generally very strong similarity with oxides plotting above the line slightly enriched in the model (Supplementary Data 1) compared with Commondale komatiite parental melt12. Oxides below the theoretical 1:1 line are underestimated in the model.

Source Data

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