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Shock transitions in silicates
The TEM identification of the spinel and beta-phase polymorphs of Mg2SiO4 in shocked meteorites, and the determination of the high strain rate mechanisms of the olivine to spinel, and spinel to beta-phase transformations. This work included the description of the first natural occurrence of beta-Mg2SiO4, which he named wadsleyite, and which is now believed to be the major constituent of the upper part of the transition zone of the Earth's mantle.
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