FeO2 and FeOOH under deep lower-mantle conditions and Earth’s oxygen–hydrogen cycles

2016/06/08 by Qingyang Hu, Duck Young Kim, Wenge Yang +5 · 5 citations
Earth and Planetary Sciences · #Geological and Geochemical Analysis #High-pressure geophysics and materials #earthquake and tectonic studies

paper · doi:10.1038/nature18018

crossref issued 2016/06/08 · crossref published 2016/06/08 · crossref published-online 2016/06/08 · openalex publication_date 2016/06/08 · crossref created 2016/06/08 · crossref published-print 2016/06/09 · crossref deposited 2023/05/18 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/23 · crossref indexed 2026/07/23

Citations

• Generalized Gradient Approximation Made Simple
• Preliminary reference Earth model
• Ab initiomolecular-dynamics simulation of the liquid-metal–amorphous-semiconductor transition in germanium
• The Redox State of Earth's Mantle
• Self-Consistent Equations Including Exchange and Correlation Effects
• Atoms, molecules, solids, and surfaces: Applications of the generalized gradient approximation for exchange and correlation

Cited by

• The pyrite-type high-pressure form of FeOOH
• Discovery of a hexagonal ultradense hydrous phase in (Fe,Al)OOH
• LDA+Usc calculations of phase relations in FeO
• Goethite [wikipedia]
• Ho-Kwang Mao [wikipedia]