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Kim, Yeongkyoo, James Kirkpatrick, R. (1996) Application of MAS NMR spectroscopy to poorly crystalline minerals: viséite. Mineralogical Magazine, 60 (403) 957-962 doi:10.1180/minmag.1996.060.403.10

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Reference TypeJournal (article/letter/editorial)
TitleApplication of MAS NMR spectroscopy to poorly crystalline minerals: viséite
JournalMineralogical MagazineISSN0026-461X
AuthorsKim, YeongkyooAuthor
James Kirkpatrick, R.Author
Year1996 (December)Volume60
Issue403
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_60/60-403-957.pdf+
DOIdoi:10.1180/minmag.1996.060.403.10Search in ResearchGate
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Mindat Ref. ID124Long-form Identifiermindat:1:5:124:3
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Full ReferenceKim, Yeongkyoo, James Kirkpatrick, R. (1996) Application of MAS NMR spectroscopy to poorly crystalline minerals: viséite. Mineralogical Magazine, 60 (403) 957-962 doi:10.1180/minmag.1996.060.403.10
Plain TextKim, Yeongkyoo, James Kirkpatrick, R. (1996) Application of MAS NMR spectroscopy to poorly crystalline minerals: viséite. Mineralogical Magazine, 60 (403) 957-962 doi:10.1180/minmag.1996.060.403.10
In(1996, December) Mineralogical Magazine Vol. 60 (403) Mineralogical Society
Abstract/NotesAbstractViséite is a poorly crystalline mineral which is difficult to study by X-ray diffraction pattern. NMR is a very useful technique to study such poorly crystalline minerals, and 31P, 27Al, and 29Si MAS NMR in conjunction with powder XRD results show that at least our Viséite sample is not a single phase with a structure analogous to that of analcime as previously reported. Rather, it is very disordered with a structure similar to that of crandallite and includes other phases including an undefined aluminophosphate, opal, and a framework aluminosilicate, probably a zeolite. The previously reported variations in the Si content of Viséite are probably due to variable amounts of opal and the framework aluminosilicate.

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