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Chinner, G. A., Sweatman, T. R. (1968) A former association of enstatite and kyanite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (284) 1052-1060 doi:10.1180/minmag.1968.036.284.03

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Reference TypeJournal (article/letter/editorial)
TitleA former association of enstatite and kyanite
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsChinner, G. A.Author
Sweatman, T. R.Author
Year1968 (December)Volume36
Issue284
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_36/36-284-1052.pdf+
DOIdoi:10.1180/minmag.1968.036.284.03Search in ResearchGate
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Mindat Ref. ID6203Long-form Identifiermindat:1:5:6203:3
GUID0
Full ReferenceChinner, G. A., Sweatman, T. R. (1968) A former association of enstatite and kyanite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (284) 1052-1060 doi:10.1180/minmag.1968.036.284.03
Plain TextChinner, G. A., Sweatman, T. R. (1968) A former association of enstatite and kyanite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (284) 1052-1060 doi:10.1180/minmag.1968.036.284.03
In(1966) Mineralogical Magazine Vol. 36 (284) Mineralogical Society
Abstract/NotesSummaryAn enstatite-cordierite-sillimanite-quartz rock from a pyroxenegranulite facies terrain in southern Rhodesia gives evidence of at least two stages of recrystallization : an early, high-pressure recrystallization to form the assemblage enstatite-kyanite-quartz, and a later, ‘retrogressive’ recrystallization during which kyanite inverted to sillimanite, and cordierite was formed by reaction. The rock itself has ratios of R2+ : Al : Si that are virtually those of cordierite ; the recent data of Schreyer (1967) may thus be applied to the occurrence. The early kyanite-enstatite recrystallization occurred under pressures in excess of 10 kb, corresponding to depths greater than those of the continental Moho.


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