Accretion and differentiation of the terrestrial planets

This will be the first of two related CEED-seminars.  The second seminar on: "Lower mantle structure developed from the chemical interaction between a basal magma ocean and the core" will be scheduled later this fall.

A background article is available at:    
http://folk.uio.no/rtronnes/Publ-sci/Tect18-Tronnes-Planet-core-mantle.pdf