Percolative Core Formation in Oxidized Planetesimals - I: Experiments on Melt Migration in Olivine Aggregates
Abstract
Major element compositions of Fe-O-S melt (Table 1) and Olivine (Table 2) in wt%. Table 3 contains dihedral angle distributions for all experimental products. The redox states of early solar system planetesimals is shown in Table 4.
Fields of Study & Subjects
Astro and Planetary Science
High-pressure geophysics and materials
Geological and Geochemical Analysis
Publication details
- Journal / source
- Mendeley Data
- Publication date
- 24 February 2026
- Language
- EN
- Document type
- Dataset