CORDIS Project
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This project investigates the processes of metal-silicate interactions and differentiation during planetary impacts, focusing on the early formation of Earth. It aims to develop models that explain core-mantle differentiation based on fluid dynamics.
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 dynamical phases involving increasingly energetic and catastrophic impacts and collisions.
The last phase of accretion, in which most of the Earth mass was accreted, involved extremely energetic collisions between already di…
Partner organizations (coordinator is shown above), with normalized type and CORDIS activity type. Guests see up to 4 partners.
France, GRENOBLE
Type: University / higher education
Activity type: Higher or Secondary Education Establishments
SME: No
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