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McConnell, Duncan (1974) Are vashegyite and kingite hydrous aluminum phyllophosphates with kaolinite-type structures ?. Mineralogical Magazine, 39 (307) 802-806 doi:10.1180/minmag.1974.039.307.08

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Reference TypeJournal (article/letter/editorial)
TitleAre vashegyite and kingite hydrous aluminum phyllophosphates with kaolinite-type structures ?
JournalMineralogical Magazine
AuthorsMcConnell, DuncanAuthor
Year1974 (September)Volume39
Issue307
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_39/39-307-802.pdf+
DOIdoi:10.1180/minmag.1974.039.307.08Search in ResearchGate
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Mindat Ref. ID6783Long-form Identifiermindat:1:5:6783:0
GUID0
Full ReferenceMcConnell, Duncan (1974) Are vashegyite and kingite hydrous aluminum phyllophosphates with kaolinite-type structures ?. Mineralogical Magazine, 39 (307) 802-806 doi:10.1180/minmag.1974.039.307.08
Plain TextMcConnell, Duncan (1974) Are vashegyite and kingite hydrous aluminum phyllophosphates with kaolinite-type structures ?. Mineralogical Magazine, 39 (307) 802-806 doi:10.1180/minmag.1974.039.307.08
In(1974, September) Mineralogical Magazine Vol. 39 (307) Mineralogical Society
Abstract/NotesSummaryIn contrast with some other hydrous aluminum phosphates, vashegyite is crystalline. Simultaneous application of several assumptions leads to the hypothesis that it has a structure analogous to that of kaolinite, and thus contains tetrahedral sheets, n[X2O5], where X is both P and H3 (in lieu of Si). Thus, the theory involving [HXO4] is extended from phosphates with isolated tetrahedral groups [XO4] and framework linkages [XO2] to sheet linkages [X2O5]. Kingite also may have a kaolinite-like structure.


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