Summary
The initial conditions of the Earth and other terrestrial planets were set 4.5 Gy ago during their accretion from the solar nebula and their concomitant differentiation into an iron-rich core and a silicate mantle. Accretion in the solar system went through several different...
More information & hyperlinks
| Web resources: | http://perso.ens-lyon.fr/renaud.deguen/ |