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Constraints on Magma Self-oxidation in Angrites and the Role of Parent-body Size

  • Authors: Hideharu Kuwahara, Damanveer S. Grewal, Kyusei Tsuno

Hideharu Kuwahara et al 2026 The Planetary Science Journal 7 .

  • Provider: AAS Journals

Caption: Figure 3.

(a) The changes in Fe3+/ΣFe ratio of residual magma during the crystallization of Group 1 angrite magma that is set by the core–mantle equilibration at 7 GPa and (b) chemical composition of the residual magma during crystallization. The pink line indicates the change in Mg# of the residual magma (Mg# = molar Mg/(Fe + Mg)×100). The pink shaded region is the Mg# range of Group 2 angrites.

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