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Finch, Adrian A., Fletcher, James G. (1992) Vitusite β€” an apatite derivative structure. Mineralogical Magazine, 56 (383) 235-239 doi:10.1180/minmag.1992.056.383.10

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Reference TypeJournal (article/letter/editorial)
TitleVitusite β€” an apatite derivative structure
JournalMineralogical MagazineISSN0026-461X
AuthorsFinch, Adrian A.Author
Fletcher, James G.Author
Year1992 (June)Volume56
Issue383
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_56/56-383-235.pdf+
DOIdoi:10.1180/minmag.1992.056.383.10Search in ResearchGate
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Mindat Ref. ID1816Long-form Identifiermindat:1:5:1816:0
GUID0
Full ReferenceFinch, Adrian A., Fletcher, James G. (1992) Vitusite β€” an apatite derivative structure. Mineralogical Magazine, 56 (383) 235-239 doi:10.1180/minmag.1992.056.383.10
Plain TextFinch, Adrian A., Fletcher, James G. (1992) Vitusite β€” an apatite derivative structure. Mineralogical Magazine, 56 (383) 235-239 doi:10.1180/minmag.1992.056.383.10
In(1992, June) Mineralogical Magazine Vol. 56 (383) Mineralogical Society
Abstract/NotesAbstractThe uncommon sodium rare-earth phosphate mineral vitusite-(Ce) (Na3RE(PO4)2) can be considered as the extreme product of sodium and rare-earth substitution in the apatite structure. Lesser amounts of substitution provide sodium and rare-earth-bearing apatites up to about 80 mol.% exchange; beyond this point vitusite is the stable phase. The structure of vitusite, determined previously from a synthetic analogue, can also be considered as a derivative from apatite, but with cations exchanged on sites normally occupied by anions. Vitusite can therefore be considered as a sodium- and rare-earthrich apatite end-member, with a distinct, but apatite-derived, structure, formed in highly persodic and high rare-earth environments. From an examination of the literature on diffusion in apatite, vitusite in principle could be formed from apatite sensu stricto by subsolidus diffusion in response to late-stage Naand RE-rich hydrothermal fluids.

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Vitusite-(Ce)


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