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Ferropericlase
Deformation of Lower-Mantle Ferropericlase (Mg,Fe)O Across the Electronic Spin Transition
The Spin State of Fe3+ in Lower Mantle Bridgmanite Ryosuke Sinmyo
Spin Crossover in Ferropericlase and Velocity Heterogeneities in the Lower Mantle
Electronic and Magnetic Structures of the Postperovskite- Type Fe[Subscript 2]O[Subscript 3] and Implications for Planetary Magnetic Records and Deep Interiors
Crystal Structures of Minerals in the Lower Mantle
Spin Transition in the Lower Mantle
5 Ringwoodite: Its Importance in Earth Sciences
The Effect of Pulsed Laser Heating on the Stability of Ferropericlase At
Elasticity of Ferropericlase and Seismic Heterogeneity in the Earth's Lower
Water Concentration in Single‐Crystal (Al,Fe)‐Bearing
A Practical Review of the Laser-Heated Diamond Anvil Cell for University Laboratories and Synchrotron Applications
Deep Mantle Melting, Global Water Circulation and Its Implications for the Stability of the Ocean Mass Shun-Ichiro Karato1* , Bijaya Karki2 and Jeffrey Park1
Ferric Iron Content of Ferropericlase As a Function of Composition, Oxygen
Spin Transitions in Mantle Minerals
Calculations of the Elastic Properties of Ferropericlase Mgfeo (X 0.25)
Viscosity Jump in the Lower Mantle Inferred from Melting Curves of Ferropericlase
Effect of Iron Content on Electrical Conductivity of Ferropericlase with Implications for the Spin Transition Pressure
Shear Waves in the Diamond-Anvil Cell Reveal Pressure-Induced Instability in (Mg,Fe)O
Top View
Discovery of Post-Perovskite and New Views on the Core–Mantle Boundary Region
Shear Waves in the Diamond-Anvil Cell Reveal Pressure-Induced Instability in (Mg,Fe)O
Equation of State and Spin Crossover of (Mg,Fe)O at High Pressure (Revision 1)
Texture Development and Slip Systems in Bridgmanite and Bridgmanite +
1 Revision 1 1 Melting Temperature Depression Due to Electronic Spin
Evidence for Complex Iron Oxides in the Deep Mantle from Feni(Cu) Inclusions in Superdeep Diamond
Iron Partitioning in Natural Lower-Mantle Minerals: Toward a Chemically Heterogeneous Lower Mantle
Natural Dissociation of Olivine to (Mg,Fe)Sio3 Perovskite And
Complete Agreement of the Post-Spinel Transition with the 660
Quantum Critical Point and Spin Fluctuations in Lower-Mantle
Melting Behavior of the Lower-Mantle Ferropericlase Across the Spin Crossover: Implication for the Ultra-Low Velocity Zones at the Lowermost Mantle
Effects of Iron on the Lattice Thermal Conductivity of Earth's Deep Mantle
Element Partitioning Between Magnesium Silicate Perovskite And
1 Elasticity of Ferropericlase Through the Pressure-Induced High-Spin
Iron Partitioning Between Ferropericlase and Bridgmanite in the Earth’S Lower Mantle
Composition and Pressure Effects on Partitioning of Ferrous Iron in Iron-Rich Lower Mantle Heterogeneities
121. Iron Isotopic Fractionation in Mineral Phases from Earth's Lower
Radiometric Temperature Measurements
Mg, Fe)Sio3 Bridgmanite (Perovskite