| Reference Type | Journal (article/letter/editorial) |
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| Title | The nature of ‘ameletite’ |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Coombs, D. S. | Author |
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| Wilkinson, J. F. G. | Author |
| Year | 1967 (September) | Volume | 36 |
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| Issue | 279 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_36/36-279-438.pdf+ |
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| DOI | doi:10.1180/minmag.1967.036.279.15Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6096 | Long-form Identifier | mindat:1:5:6096:1 |
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| GUID | 0 |
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| Full Reference | Coombs, D. S., Wilkinson, J. F. G. (1967) The nature of ‘ameletite’. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (279) 438-443 doi:10.1180/minmag.1967.036.279.15 |
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| Plain Text | Coombs, D. S., Wilkinson, J. F. G. (1967) The nature of ‘ameletite’. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (279) 438-443 doi:10.1180/minmag.1967.036.279.15 |
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| In | (1966) Mineralogical Magazine Vol. 36 (279) Mineralogical Society |
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| Abstract/Notes | SummaryOriginally described in phonolitic rocks from the Dunedin district, New Zealand, ameletite was considered by Marshall (1929) to be a chlorine-bearing sodium aluminium silicate, probably a feldspathoid, and later, a zeolite of unspecified composition. Optical, X-ray, and chemical data on several ‘ameletite’-bearing felsic volcanic rocks from the type area indicate that material previously designated as ameletite is variously nepheline and mixtures of sodalite, analcime, phillipsite, and nepheline. Criteria thought to be characteristic of ameletite are discussed. |
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