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- W2068943635 abstract "We report new shock-compression data for polycrystalline (Mg,Fe)O up to 130 GPa shock pressures corresponding to Earth's lowermost mantle conditions. Our data together with the existing shock-wave data of (Mg,Fe)O and its end-members MgO and FeO reveal that the Hugoniot curves of (Mg,Fe)O does not change with varying FeO content for their B1 phase (NaCl-structure) in the pressure–relative-volume plane. The evidence of the volume change within 3% at around 120 GPa along the Hugoniot of (Mg0.6, Fe0.4)O is consistent with a structural transition from B1 phase (NaCl cubic) to B8 phase (NiAs-type hexagonal). Such a structural transition of (Mg,Fe)O, if indeed occurs, may in part contribute to the scattering of seismic waves and change in velocity gradient found in the lowermost mantle." @default.
- W2068943635 created "2016-06-24" @default.
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- W2068943635 date "2006-10-26" @default.
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- W2068943635 title "Shock Compression and Phase Transitions of Magnesiowüstite (Mg,Fe)O up to Earth's Lowermost Mantle Conditions" @default.
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- W2068943635 doi "https://doi.org/10.1088/0256-307x/23/11/045" @default.
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