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Duffin, W. J., Goodyear, J. (1960) A thermal and X-ray investigation of scarbroite. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (248) 353-362 doi:10.1180/minmag.1960.032.248.01

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Reference TypeJournal (article/letter/editorial)
TitleA thermal and X-ray investigation of scarbroite
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsDuffin, W. J.Author
Goodyear, J.Author
Year1960 (March)Volume32
Page(s)353-362Issue248
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_32/32-248-353.pdf+
DOIdoi:10.1180/minmag.1960.032.248.01
Mindat Ref. ID5547Long-form Identifiermindat:1:5:5547:9
GUID63795097-ceab-4b11-9afd-72be93ea1529
Full ReferenceDuffin, W. J., Goodyear, J. (1960) A thermal and X-ray investigation of scarbroite. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (248) 353-362 doi:10.1180/minmag.1960.032.248.01
Plain TextDuffin, W. J., Goodyear, J. (1960) A thermal and X-ray investigation of scarbroite. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (248) 353-362 doi:10.1180/minmag.1960.032.248.01
In(1959) Mineralogical Magazine Vol. 32 (248) Mineralogical Society
Abstract/NotesSummaryScarbroite, a fine-grained but compact deposit obtained from fissures in the sandstone on the north Yorkshire coast, is shown by chemical analysis to have an idealized formula Al2(CO3)3路12Al(OH)3. X-ray and electron diffraction data indicate a triclinic cell with a 9路94 脜., b 14路88 脜., c 26路47 脜., 伪 98路7掳, 尾 96路5掳, and 纬 89路0掳. A layer structure consisting of gibbsite-type sheets of Al(OH)3 and sheets of Al2(CO3)3 is proposed. The structure is stable from room temperature to about 125掳 C.


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