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14 h 00 min

Séminaire de Renaud Deguen

12 March à 14 h 00 min - 17 h 00 min

"Dynamics of core-mantle differentiation and equilibration" The basic structure of the terrestrial planets - an iron-rich metallic core surrounded by a silicate mantle - has been set during the accretion of the planets, when the high temperature allowed the metal and silicate phases to melt and separate. The amount of transfert of chemical elements and […]

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