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Taylor, H. F. W. (1969) Segregation and cation-ordering in sjögrenite and pyroaurite. Mineralogical Magazine, 37 (287) 338-342 doi:10.1180/minmag.1969.037.287.04

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Reference TypeJournal (article/letter/editorial)
TitleSegregation and cation-ordering in sjögrenite and pyroaurite
JournalMineralogical Magazine
AuthorsTaylor, H. F. W.Author
Year1969 (September)Volume37
Issue287
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_37/37-287-338.pdf+
DOIdoi:10.1180/minmag.1969.037.287.04Search in ResearchGate
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Mindat Ref. ID6293Long-form Identifiermindat:1:5:6293:4
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Full ReferenceTaylor, H. F. W. (1969) Segregation and cation-ordering in sjögrenite and pyroaurite. Mineralogical Magazine, 37 (287) 338-342 doi:10.1180/minmag.1969.037.287.04
Plain TextTaylor, H. F. W. (1969) Segregation and cation-ordering in sjögrenite and pyroaurite. Mineralogical Magazine, 37 (287) 338-342 doi:10.1180/minmag.1969.037.287.04
In(1969, September) Mineralogical Magazine Vol. 37 (287) Mineralogical Society
Abstract/NotesSummaryA specimen from Långban, Sweden, was found to consist largely of sjögrenite in which segregation and ordering of the metal cations had occurred, yielding an intergrowth of regions of two main types with compositions probably of or near Mg2/3Fe1/3(OH)2(CO3)1/6(H2O)0·4 and Mg12/13Fe1/13(OH)2(CO3)1/26(H2O)0·8. To a smaller extent segregation had proceeded further, giving regions probably approximating to the end-member Mg(OH)2.H2O. It is suggested that the names sjögrenite and pyroaurite be used for the 2H- and 3R- polytypes of this structure irrespective of Mg:Fe ratio, segregation, or cation ordering.

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