The magnesiow�stite: iron equilibrium and its implications for the activity-composition relations of (Mg,Fe)2SiO4 olivine solid solutions

2003/12/01 by Hugh St. C. O'Neill, Hugh O’Neill, Mark I. Pownceby +2 · 47 citations
Chemistry · Earth and Planetary Sciences · Materials Science · #Analytical Chemistry (journal) #Chemistry #Clay minerals and soil interactions #Crystallography #Geological and Geochemical Analysis #High-pressure geophysics and materials #Magnetite #Materials science #Metal #Metallurgy #Mineralogy #Mössbauer spectroscopy #Physics #Solid solution #Thermodynamics #Wüstite

paper · doi:10.1007/s00410-003-0496-4

published in Contributions to Mineralogy and Petrology 146(3), 308-325 (Springer Science+Business Media)

openalex publication_date 2003/12/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/25

Citations

• Zur Theorie des Durchgangs schneller Korpuskularstrahlen durch Materie
• A convenient method for measuring ferric iron in magnesiowustite (MgO-Fe (sub 1-x) O)

Cited by

• High-pressure phase relations in the Mg–Fe–O system and the conditions at which ferropericlase inclusions in diamonds are formed
• Viscosity jump in the lower mantle inferred from melting curves of ferropericlase. [europepmc]