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- W2045674003 abstract "The phase boundary between ringwoodite and perovskite plus periclase in Mg2SiO4 was determined at 1600 °C under hydrous conditions with 1∼3 wt% H2O. We found that the boundary moved to high-pressure side by ∼0.2 GPa in these hydrous conditions compared with that in anhydrous condition. The SIMS measurements confirmed that the ringwoodite in hydrous condition contained a significant amount (∼1 wt%) of water, whereas the perovskite accepted only very little (∼0.05 wt%) water in its crystal structure. The discrepancy between the pressure of 660 km seismic discontinuity and that of the postspinel transformation reported in a recent in situ x-ray study is not explained by the effect of water on the transformation." @default.
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- W2045674003 date "2001-09-15" @default.
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- W2045674003 title "Effect of water on the spinel-postspinel transformation in Mg<sub>2</sub>SiO<sub>4</sub>" @default.
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- W2045674003 doi "https://doi.org/10.1029/2001gl013194" @default.
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