Fig. 5
Download original image
Top: core densities vs. fO2 for compositions considered in this study compared to densities of minerals, meteorites, and Psyche. Bottom: change in bulk density for different amounts of mantle stripping. Densities are calculated by mass balance. Sources of initial densities: meteoritic (Britt et al. 2002; Macke et al. 2011; Ostrowski & Bryson 2019), Psyche (Farnocchia et al. 2024), and minerals (Dziewonski & Anderson 1981; Hauck & Johnson 2019; Zhu et al. 2021). A density of 2.2 g/cm3 is the minimum plausible mantle density.
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.