Accretion and differentiation of the terrestrial planets

by

Reidar Trønnes

Centre for Earth Evolution and Dynamics

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
 

Published Sep. 19, 2018 11:31 AM - Last modified Oct. 1, 2018 9:35 AM