Mg-Fe-2+-Fe3+-Al-Si-O phase relations at lower mantle conditions: Lack of evidence for Fe-disproportionation (2007)

First Author: L Armstrong

Attributed to: How did Earth's Mantle Become Oxidized? The Role of Perovskite Crystal Chemistry in Earth's Evolution funded by NERC

No abstract provided

Type: Conference/Paper/Proceeding/Abstract

Volume: 71

Issue: 15