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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 A1.

Temperature conditions used for calculation of fO2. Solidus temperature shown as H2000 was taken from C. Herzberg et al. (2000). Liquidus temperature shown as H&Z1996; A2018 was taken from C. Herzberg & J. Zhang (1996) and D. Andrault et al. (2018). Temperature at the CMEP shown as R2015 was taken from D. C. Rubie et al. (2015).

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