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- W2023584231 abstract "Very marked differences in the metastable persistence of coesite and stishovite have been demonstrated; the former possibly persists indefinitely below 1000°C at 1 atmosphere dry, and the latter completely decomposes in minutes above 500° to 600°C to an amorphous or short range order phase. Quartz was grown (metastably) at temperatures well above its stability field from both coesite and stishovite, possibly by way of a short range order phase. The absence of stishovite in meteor-impact craters cannot be taken as evidence that it was not formed. If it has reversed in normal natural environments the product would almost certainly be a short range order phase or derivative." @default.
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- W2023584231 date "1963-05-31" @default.
- W2023584231 modified "2023-10-14" @default.
- W2023584231 title "Coesite and Stishovite: Stepwise Reversal Transformations" @default.
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- W2023584231 doi "https://doi.org/10.1126/science.140.3570.991" @default.
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