| Reference Type | Journal (article/letter/editorial) |
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| Title | Some crystallographic studies in the system CaSOa4-CaSO4.2H2O I. The polymorphism of anhydrous CaSO4 |
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| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
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| Authors | Gay, P. | Author |
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| Year | 1965 (June) | Volume | 35 |
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| Issue | 270 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_35/35-270-347.pdf+ |
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| DOI | doi:10.1180/minmag.1965.035.270.08Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 5877 | Long-form Identifier | mindat:1:5:5877:7 |
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| GUID | 0 |
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| Full Reference | Gay, P. (1965) Some crystallographic studies in the system CaSOa4-CaSO4.2H2O I. The polymorphism of anhydrous CaSO4. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 347-353 doi:10.1180/minmag.1965.035.270.08 |
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| Plain Text | Gay, P. (1965) Some crystallographic studies in the system CaSOa4-CaSO4.2H2O I. The polymorphism of anhydrous CaSO4. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 347-353 doi:10.1180/minmag.1965.035.270.08 |
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| In | (1965) Mineralogical Magazine Vol. 35 (270) Mineralogical Society |
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| Abstract/Notes | SummaryThe existence and relationships of the polymorphs of CaSO4 have been studied by X-ray methods. Only two distinct phases are found: no crystallographic evidence is available to support the suggestion that the γ-CaSO4 structure can have two forms, and it is shown that most previous data on the existence of the high temperature α-CaSO4 polymorphs are likely to be due to decomposition of the sulphate.Some observations on the γ to β-CaSO4 transformation are reported. The structural implications of these results and their relevance to the nature of the transformation are discussed. |
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