Physical Review Letters · 1992 · 31 citations · 23 references
Natural SciencesMaterials EngineeringMaterials ScienceCrystal StructureMineralogySolid State PhysicsAmorphous MaterialsAmorphous SolidsCrystalline MaterialsCrystallographyElectron MicroscopyX-ray CrystallographyAmbient Temperature EffectsAmorphous Phase ContentAmorphous Solid FormationHigh-resolution Electron MicroscopyHigh-resolution Transmission Electron MicroscopySilicate GlassesSilicate Melt Structure
\ensuremath{\alpha}-quartz becomes x-ray amorphous when compressed, at ambient temperature, by pressures of 25 to 30 GPa. [Hemley et al. Nature 334, 5 (1988)]. The relationship between pressure-amorphized and melt-quenched silica is of great interest. The most fundamental characteristic of melt-quenched silica is its lack of periodicity at the atomic level. We report here that high-resolution electron microscopy shows that \ensuremath{\alpha}-quartz, pressure amorphized at 30.5 GPa is, as is conventional melt-quenched silica, amorphous at the atomic level.
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High‐Pressure Research in Mineral Physics
Robert M. Hazen · Eos · 1988 · 971 citations
Medium-range structural order in covalent amorphous solids
Stephen R. Elliott · Nature · 1991 · 692 citations
Pressure-induced amorphization of crystalline silica
Russell J. Hemley, A. P. Jephcoat, H. K. Mao et al. · Nature · 1988 · 617 citations
Natural Sciences, Materials Engineering, Materials Science +14
Glasses and the vitreous state
Giovanni Aliprandi · Materials Chemistry and Physics · 1992 · 302 citations