Effects of Fe spin transition on the elasticity of (Mg, Fe) O magnesiowustites and implications for the seismological properties of the Earth's lower mantle
High-pressure x-ray diffraction of (Mg0.80 Fe0.20)O at room temperature reveals a discontinuity in the bulk modulus at 40 (±5) GPa, similar to the pressure at which an electronic spin-pairing transition of Fe2+ is observed by Mössbauer spectroscopy. We determine the zero-pressure bulk modulus of low...
Váldodahkkit: | Speziale, S, Lee, V, Clark, S, Lin, J, Pasternak, M, Jeanloz, R |
---|---|
Materiálatiipa: | Journal article |
Giella: | English |
Almmustuhtton: |
2007
|
Geahča maid
-
Iron spin transition in Earth's mantle.
Dahkki: Speziale, S, et al.
Almmustuhtton: (2005) -
High Sodium Solubility in Magnesiowüstite in Iron‐Rich Deep Lower Mantle
Dahkki: Susannah M. Dorfman, et al.
Almmustuhtton: (2024-06-01) -
Broad elastic softening of (Mg,Fe)O ferropericlase across the iron spin crossover and a mixed-spin lower mantle
Dahkki: Méndez, ASJ, et al.
Almmustuhtton: (2022) -
Spin Transition of Iron in δ‐(Al,Fe)OOH Induces Thermal Anomalies in Earth's Lower Mantle
Dahkki: Wen‐Pin Hsieh, et al.
Almmustuhtton: (2020-02-01) -
HIGH-TEMPERATURE ELECTRICAL-CONDUCTIVITY OF THE LOWER-MANTLE PHASE (MG,FE)O
Dahkki: Wood, B, et al.
Almmustuhtton: (1991)