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Gellatly, D. C. (1966) Graphite in natural and experimental carbonate systems. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (275) 963-970 doi:10.1180/minmag.1966.035.275.08

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Reference TypeJournal (article/letter/editorial)
TitleGraphite in natural and experimental carbonate systems
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsGellatly, D. C.Author
Year1966 (September)Volume35
Issue275
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_35/35-275-963.pdf+
DOIdoi:10.1180/minmag.1966.035.275.08Search in ResearchGate
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Mindat Ref. ID5997Long-form Identifiermindat:1:5:5997:2
GUID0
Full ReferenceGellatly, D. C. (1966) Graphite in natural and experimental carbonate systems. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (275) 963-970 doi:10.1180/minmag.1966.035.275.08
Plain TextGellatly, D. C. (1966) Graphite in natural and experimental carbonate systems. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (275) 963-970 doi:10.1180/minmag.1966.035.275.08
In(1965) Mineralogical Magazine Vol. 35 (275) Mineralogical Society
Abstract/NotesSummaryGraphite occurs in the Darkainle nepheline syenite complex, Somali Republic, as small drop-like grains in an altered ankeritic carbonatite; it has been recorded previously from carbonate-bearing nepheline syenites and kimberlites. Experimental evidence indicates that siderite decomposes to a stable association of magnetite and graphite within the PT ranges 500 to 10 000 bars and 455 to 745° C. The graphite in carbonatite and other alkaline igneous rocks may have been formed similarly by the decomposition of siderite or iron-rich carbonates.

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Williams, D. W. (1966) Externally heated cold-seal pressure vessels for use to 1200° C at 1000 bars. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (275) 1003-1012 doi:10.1180/minmag.1966.035.275.14
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