Pressure-induced amorphization in {α}-quartz has been investigated using constant-pressure molecular-dynamics calculations with the two-body potential of van Beest, Kramer, and van Santen. Both the static properties and the crystalline-to-amorphous phase transition were very well reproduced. Through an analysis of the elastic moduli, the mechanism for the transformation is shown to be a mechanical instability driven mainly by a cooperative twisting and compression of the helical tetrahedral silicate units with an abrupt decrease in the C₁₂, C₂₃, C₁₃, C₁₄, and C₃₃ elastic moduli.
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Tse et al. (1991) studied this question.
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