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Geiger, C. A., Winkler, B., Langer, K. (1989) Infrared spectra of synthetic almandine–grossular and almandine–pyrope garnet solid solutions: evidence for equivalent site behaviour. Mineralogical Magazine, 53 (370) 231-237 doi:10.1180/minmag.1989.053.370.10

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Reference TypeJournal (article/letter/editorial)
TitleInfrared spectra of synthetic almandine–grossular and almandine–pyrope garnet solid solutions: evidence for equivalent site behaviour
JournalMineralogical MagazineISSN0026-461X
AuthorsGeiger, C. A.Author
Winkler, B.Author
Langer, K.Author
Year1989 (April)Volume53
Issue370
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_53/53-370-231.pdf+
DOIdoi:10.1180/minmag.1989.053.370.10Search in ResearchGate
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Mindat Ref. ID1496Long-form Identifiermindat:1:5:1496:4
GUID0
Full ReferenceGeiger, C. A., Winkler, B., Langer, K. (1989) Infrared spectra of synthetic almandine–grossular and almandine–pyrope garnet solid solutions: evidence for equivalent site behaviour. Mineralogical Magazine, 53 (370) 231-237 doi:10.1180/minmag.1989.053.370.10
Plain TextGeiger, C. A., Winkler, B., Langer, K. (1989) Infrared spectra of synthetic almandine–grossular and almandine–pyrope garnet solid solutions: evidence for equivalent site behaviour. Mineralogical Magazine, 53 (370) 231-237 doi:10.1180/minmag.1989.053.370.10
In(1989, April) Mineralogical Magazine Vol. 53 (370) Mineralogical Society
Abstract/NotesAbstractThe infrared (IR) spectra of almandine-grossular and almandine-pyrope garnet solid solutions have been measured using the powder method. Frequency shifts of a band related to internal vibrations associated with the 8-co-ordinate dodecahedral site are nonlinear in almandine-grossular garnets and mimic the form of its molar volume of mixing curve. Almandine-pyrope solid solutions have nearly ideal molar volumes of mixing and the frequency shift of this same 8-co-ordinate site-related band is linear. The IR data support the empirically based crystal chemical model of Equivalent Site (ES) behaviour (Newton and Wood, 1980). The IR spectra give no indication of long-range ordering between Ca and Fe2+ in garnet, but thermodynamic calculations involving Ca-poor garnets might be affected by small volume or short-range ordering anomalies.


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