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- W2605495341 abstract "Dehydration and recrystallization of fine and coarse powders and massive samples of garnierite under heating conditions in air were observed by means of X-ray diffraction analysis with the aid of infrared absorption analysis and solvent extraction. The rate of recrystallization of garnierite to olivine was shown to be an inverse relationship to the rate of dehydration. This result is interpreted in connection with the destruction inflicted on the crystal structure of garnierite; that is the more slowly this reaction occurs, the more readily olivine is formed as a result of the topotactic reaction between olivine and garnierite.Moreover these experimental data showed that at the temperature range between 670°C and 720°C the garnierite phase shifts to an X-ray amorphous phase which would be formed by the oxidizing reaction of garnierite, prior to the formation of olivine. The formation of amorphous phase was deduced from infrared absorption spectra of silicate glasses studied by Yanagase and Suginohara. The formation of olivine and pyroxene was considered in relation to a reaction mechanism proposed by Brindley, Taylor and Hayami." @default.
- W2605495341 created "2017-04-28" @default.
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- W2605495341 date "1975-01-01" @default.
- W2605495341 modified "2023-09-25" @default.
- W2605495341 title "Formation of Olivine and Pyroxene from Garnierite" @default.
- W2605495341 doi "https://doi.org/10.2473/shigentosozai1953.91.1050_541" @default.
- W2605495341 hasPublicationYear "1975" @default.
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