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Kinomura, N., Kume, S., Koizumi, M. (1975) Synthesis of K2SiSi3O9 with silicon in 4- and 6-coordination. Mineralogical Magazine, 40 (312) 401-404 doi:10.1180/minmag.1975.040.312.09

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Reference TypeJournal (article/letter/editorial)
TitleSynthesis of K2SiSi3O9 with silicon in 4- and 6-coordination
JournalMineralogical Magazine
AuthorsKinomura, N.Author
Kume, S.Author
Koizumi, M.Author
Year1975 (December)Volume40
Issue312
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_40/40-312-401.pdf+
DOIdoi:10.1180/minmag.1975.040.312.09Search in ResearchGate
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Mindat Ref. ID6896Long-form Identifiermindat:1:5:6896:7
GUID0
Full ReferenceKinomura, N., Kume, S., Koizumi, M. (1975) Synthesis of K2SiSi3O9 with silicon in 4- and 6-coordination. Mineralogical Magazine, 40 (312) 401-404 doi:10.1180/minmag.1975.040.312.09
Plain TextKinomura, N., Kume, S., Koizumi, M. (1975) Synthesis of K2SiSi3O9 with silicon in 4- and 6-coordination. Mineralogical Magazine, 40 (312) 401-404 doi:10.1180/minmag.1975.040.312.09
In(1975, December) Mineralogical Magazine Vol. 40 (312) Mineralogical Society
Abstract/NotesSummaryTwo kinds of vitreous material with composition K2GeSi3O9 and K2Si4O9 were treated under conditions of high temperature and pressure. The X-ray diffraction patterns of the products were similar to that of K2TiSi3O9, which has the wadeite, K2ZrSi3O9, structure.A natural crystal of K-feldspar was also treated under the same conditions. The product was found to consist of three phases, coesite, kyanite, and the above-mentioned K2Si4O9. Since Zr ions in wadeite are in a 6-coordinated site, one-quarter of Si ions in K2Si4O9 are considered to be in 6-coordination. This is the first silicate in which Si ions occupy sites of 4- and 6-coordinations in one crystal at the same time.


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