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Phillips, Wm. Revell (1963) A differential thermal study of the chlorites. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (260) 404-414 doi:10.1180/minmag.1963.033.260.06

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Reference TypeJournal (article/letter/editorial)
TitleA differential thermal study of the chlorites
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsPhillips, Wm. RevellAuthor
Year1963 (March)Volume33
Page(s)404-414Issue260
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_33/33-260-404.pdf+
DOIdoi:10.1180/minmag.1963.033.260.06Search in ResearchGate
Mindat Ref. ID5717Long-form Identifiermindat:1:5:5717:6
GUID787f4fa4-9a5c-4c93-aca6-3887f6e8c48e
Full ReferencePhillips, Wm. Revell (1963) A differential thermal study of the chlorites. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (260) 404-414 doi:10.1180/minmag.1963.033.260.06
Plain TextPhillips, Wm. Revell (1963) A differential thermal study of the chlorites. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (260) 404-414 doi:10.1180/minmag.1963.033.260.06
In(1962) Mineralogical Magazine Vol. 33 (260) Mineralogical Society
Abstract/NotesSummaryDifferential thermal analysis alone appears inadequate as a tool for distinguishing the many chlorite varieties; however, this process is capable of yielding much valuable information about the chlorites. The 7 Ã… septechlorite structure may be easily distinguished from the normal 14 Ã… chlorite structure. Two stages of dehydration, oxidation of ferrous iron, and structural collapse appear as endothermic and exothermic peaks on the D.T.A. chlorite curves. Septechlorites show only one, large dehydration stage, which leads directly to the structural breakdown. Iron oxidation accompanies the initial dehydration in both structural types, and the temperature at which dehydration begins is noticeably lowered by increasing ferrous iron content of the chlorite variety.


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