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- W2038706875 abstract "We have heated magnesiowustites (Mg 0.5 Fe 0.5 )O and (Mg 0.8 Fe 0.2 )O to temperatures of over 1000 K at pressures of over 80 GPa simulating the stability of the solid solution at physical conditions relevant to the Earth9s lower mantle. The X-ray study of the externally heated samples in diamond-anvil cells shows that magnesiowustite may dissociate into a magnesium-rich and an iron-rich oxide component. The result is important because the decomposition of magnesiowustite into lighter and heavier phases will cause dynamic effects that could lead to mantle heterogeneity." @default.
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- W2038706875 date "2001-10-01" @default.
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- W2038706875 title "Stability of (Mg0.5Fe0.5)O and (Mg0.8Fe0.2)O magnesiowüstites in the lower mantle" @default.
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- W2038706875 doi "https://doi.org/10.1127/0935-1221/2001/0013-0857" @default.
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