| Reference Type | Journal (article/letter/editorial) |
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| Title | A zinc phosphate analogue of analcime: kehoeite |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | McConnell, Duncan | Author |
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| Year | 1964 (March) | Volume | 33 |
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| Issue | 264 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_33/33-264-799.pdf+ |
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| DOI | doi:10.1180/minmag.1964.033.264.08Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5785 | Long-form Identifier | mindat:1:5:5785:5 |
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| GUID | 0 |
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| Full Reference | McConnell, Duncan (1964) A zinc phosphate analogue of analcime: kehoeite. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (264) 799-803 doi:10.1180/minmag.1964.033.264.08 |
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| Plain Text | McConnell, Duncan (1964) A zinc phosphate analogue of analcime: kehoeite. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (264) 799-803 doi:10.1180/minmag.1964.033.264.08 |
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| In | (1962) Mineralogical Magazine Vol. 33 (264) Mineralogical Society |
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| Abstract/Notes | SummaryKehoeite, a hydrated zinc aluminate-phosphate, produces an X-ray powder diffraction pattern with interplanar spacings similar to those of analcime, viséite, and pollucite. The diffraction maxima appear to be compatible with a cubic (or pseudocubic) lattice with a 13·7 Å. It is concluded that kehoeite is essentially isostructural with analcime and that its framework is composed of linked tetrahedra: (AlO2)−, (H3O2)−, and (PO2)+, as was found to be the case for viséite, which contains (SiO2) in addition. Calculations of the density, the number of oxygens in the unit cell, and the chemical composition are consistent with the structural formula Zn5·5Ca2·5(H2O)32[(Al16P16(H3)16)O96]. |
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