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 |
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Materiálatiipa: | Journal article |
Giella: | English |
Almmustuhtton: |
2007
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Geahča maid
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Iron spin transition in Earth's mantle.
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