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Wadsleyite (β-(Mg,Fe)2SiO4) is known to accept variable amounts of H, and may be an important reservoir of H in the transition zone of the mantle. The crystal structure of Fo94.6 hydrous wadsleyite (Mg1.730Fe0.098 Al0.008Si0.991H0.355O4) synthesized at 1400 oC and 17GPa has been refined in space group I2/m from 1784 measured intensities of which 830 were(More)
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