| Reference Type | Journal (article/letter/editorial) |
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| Title | Some natural analcime solid solutions |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Wilkinson, J. F. G. | Author |
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| Year | 1963 (June) | Volume | 33 |
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| Issue | 261 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_33/33-261-498.pdf+ |
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| DOI | doi:10.1180/minmag.1963.033.261.06Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5731 | Long-form Identifier | mindat:1:5:5731:2 |
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| GUID | 0 |
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| Full Reference | Wilkinson, J. F. G. (1963) Some natural analcime solid solutions. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (261) 498-505 doi:10.1180/minmag.1963.033.261.06 |
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| Plain Text | Wilkinson, J. F. G. (1963) Some natural analcime solid solutions. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (261) 498-505 doi:10.1180/minmag.1963.033.261.06 |
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| In | (1962) Mineralogical Magazine Vol. 33 (261) Mineralogical Society |
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| Abstract/Notes | SummaryChemical, optical, and X-ray data are presented on three analcimes from a differentiation sequence, olivine-theralite to analcime-tinguaite; compared with the ideal analcime composition, they reveal replacement of NaAl→Si. Optical and X-ray data on these minerals accord reasonably well with analcimes possessing similar compositions, and synthesized in the sub-solidus region in the NaAlSiO4-NaAlSi3O8-H2O system. |
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