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Tomkeieff, S. I. (1926) On some chloritic minerals associated wlth the basaltic Carboniferous rocks of Derbyshire. Mineralogical Magazine and Journal of the Mineralogical Society, 21 (114) 73-82 doi:10.1180/minmag.1926.021.114.02

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Reference TypeJournal (article/letter/editorial)
TitleOn some chloritic minerals associated wlth the basaltic Carboniferous rocks of Derbyshire
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsTomkeieff, S. I.Author
Year1926 (September)Volume21
Issue114
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_21/21-114-73.pdf+
DOIdoi:10.1180/minmag.1926.021.114.02
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Mindat Ref. ID7020Long-form Identifiermindat:1:5:7020:5
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Full ReferenceTomkeieff, S. I. (1926) On some chloritic minerals associated wlth the basaltic Carboniferous rocks of Derbyshire. Mineralogical Magazine and Journal of the Mineralogical Society, 21 (114) 73-82 doi:10.1180/minmag.1926.021.114.02
Plain TextTomkeieff, S. I. (1926) On some chloritic minerals associated wlth the basaltic Carboniferous rocks of Derbyshire. Mineralogical Magazine and Journal of the Mineralogical Society, 21 (114) 73-82 doi:10.1180/minmag.1926.021.114.02
In(1926) Mineralogical Magazine Vol. 21 (114) Mineralogical Society
Abstract/NotesThe occurrence of chloritic minerals as infillings of vesicular cavities in volcanic rocks is very common in rocks of all geological ages. Numerous chlorites have been described and analysed, but their classification and nomenclature are complicated by the fact that, as in the case with other hydrous alumino-silicates such as zeolites and clay minerals, the chloiites present a great variety of chemical compounds, usually of indefinite composition.


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