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Earth and Mars Interior Structures Set by Remelting of the First Solid Mantle

  • Authors: Antonio Manjón-Cabeza Córdoba, Maxim D. Ballmer, Oliver Shorttle

Antonio Manjón-Cabeza Córdoba et al 2026 The Astrophysical Journal Letters 1005 .

  • Provider: AAS Journals

Caption: Figure 2.

Earth and Mars cases showing different crystallization timescales as lines. Black lines are reference (average) cases with η = 1018, Fe# = 10 and 20, and core temperatures of 4400 and 2400 K (respectively for Earth and Mars). For the properties we explore and associated references, see text. (a) Maximum Fe# for a given crystallization timescale. (b) Resulting density difference of the buffered layer as a function of the crystallization timescale.

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