Abstract: Ultrahigh-pressure structure of GeO<sub>2</sub> glass with coordination number >6: implications for structure of magma at the core-mantle boundary (2016 AGU Fall Meeting)

Ultrahigh-pressure structure of GeO₂ glass with coordination number >6: implications for structure of magma at the core-mantle boundary

Yoshio Kono, Carnegie Institution for Science Washington, Washington, DC, United States, Curtis Kenney-Benson, HPCAT, Carnegie Institution of Washington, Advanced Photon Source, Argonne National Laboratory, Argonne, IL, United States, Daijo Ikuta, Tohoku University, Sendai, Japan, Yuki Shibazaki, Tohoku University, Frontier Research Institute for Interdisciplinary Sciences, Sendai, Japan, Yanbin Wang, University of Chicago, Chicago, IL, United States and Guoyin Shen, Carnegie Institution for Science, Washington, DC, United States

Back to: Physics and Chemistry of the Deep Earth I

Ultrahigh-pressure structure of GeO2 glass with coordination number >6: implications for structure of magma at the core-mantle boundary

Ultrahigh-pressure structure of GeO₂ glass with coordination number >6: implications for structure of magma at the core-mantle boundary