| Reference Type | Journal (article/letter/editorial) |
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| Title | The cummingtonite problem |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Layton, W. | Author |
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| Phillips, R. | Author |
| Year | 1960 (December) | Volume | 32 |
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| Issue | 251 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_32/32-251-659.pdf+ |
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| DOI | doi:10.1180/minmag.1960.032.251.08 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5594 | Long-form Identifier | mindat:1:5:5594:3 |
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| GUID | 0 |
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| Full Reference | Layton, W., Phillips, R. (1960) The cummingtonite problem. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (251) 659-663 doi:10.1180/minmag.1960.032.251.08 |
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| Plain Text | Layton, W., Phillips, R. (1960) The cummingtonite problem. Mineralogical Magazine and Journal of the Mineralogical Society, 32 (251) 659-663 doi:10.1180/minmag.1960.032.251.08 |
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| In | (1959) Mineralogical Magazine Vol. 32 (251) Mineralogical Society |
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| Abstract/Notes | SummaryAn examination of available chemical analyses shows that the anthophyllite and cummingtonite series of amphibole minerals are not isodimorphous. Whilst the anthophyllites are truly lime-free amphiboles, small amounts of calcium are essential to stabilize the monoclinic lattice of cummingtonites, which should be regarded as lime-poor amphiboles, analogous to the lime-poor pyroxenes. The existence of synthetic clino-anthophyllites is considered. |
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