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• W1655474200 abstract "Pressure-induced amorphization (PIA) in the solid state (i.e., without melting) is a well-known process that has been experimentally observed for several materials and minerals1−2, including α-quartz1−4. Apart from meteorite impacts, it has been predicted as irrelevant under natural P-T conditions because it can develop only under high pressures (e.g., 15–40 GPa for α-quartz1−4,6), in metastable materials, either at very low temperature or during a shock. Such pressures can only be found at extreme depths within the Earth, at which crystal-crystal transitions are expected rather than amorphization1−2, because of the high temperatures." @default.
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• W1655474200 date "2010-05-01" @default.
• W1655474200 modified "2023-09-26" @default.
• W1655474200 title "Incipient amorphization of metastable α-quartz induced by ultrahigh pressure (>15 GPa?): first report in an eclogite" @default.
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