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Dunn, Pete J., Peacor, Donald R., Nelen, Joseph E., Ramik, Robert A. (1983) Ganophyllite from Franklin, New Jersey; Pajsberg, Sweden; and Wales new chemical data. Mineralogical Magazine, 47 (345) 563-566 doi:10.1180/minmag.1983.047.345.18

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Reference TypeJournal (article/letter/editorial)
TitleGanophyllite from Franklin, New Jersey; Pajsberg, Sweden; and Wales new chemical data
JournalMineralogical MagazineISSN0026-461X
AuthorsDunn, Pete J.Author
Peacor, Donald R.Author
Nelen, Joseph E.Author
Ramik, Robert A.Author
Year1983 (December)Volume47
Issue345
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_47/47-345-563.pdf+
DOIdoi:10.1180/minmag.1983.047.345.18Search in ResearchGate
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Mindat Ref. ID3571Long-form Identifiermindat:1:5:3571:6
GUID0
Full ReferenceDunn, Pete J., Peacor, Donald R., Nelen, Joseph E., Ramik, Robert A. (1983) Ganophyllite from Franklin, New Jersey; Pajsberg, Sweden; and Wales new chemical data. Mineralogical Magazine, 47 (345) 563-566 doi:10.1180/minmag.1983.047.345.18
Plain TextDunn, Pete J., Peacor, Donald R., Nelen, Joseph E., Ramik, Robert A. (1983) Ganophyllite from Franklin, New Jersey; Pajsberg, Sweden; and Wales new chemical data. Mineralogical Magazine, 47 (345) 563-566 doi:10.1180/minmag.1983.047.345.18
In(1983, December) Mineralogical Magazine Vol. 47 (345) Mineralogical Society
Abstract/NotesAbstractGanophyllite from Franklin, New Jersey, Pajsberg, Sweden, and the Benallt Mine, Wales, has been chemically reinvestigated. Twelve new analyses confirm the general structure of Kato (1980) and yield the tentative formula (K,Na,Ca)2Mn8(Si,Al)12(O,OH)32(OH)4·8H2O. There is little solid solution among octahedral cations, and the Si:Al ratio is nearly constant at 10:2. Ca and (Na + K) are apparently differentiated, but all examined ganophyllites are K-rich. Much of the water content is loosely bound and the upper limit of water content is not well defined. Ganophyllite is relatively invariant in chemical composition from locality to locality.


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