Abstract
Summary: The existence and relationships of the polymorphs of CaSO4have been studied by X-ray methods. Only two distinct phases are found: no crystallographic evidence is available to support the suggestion that theγ-CaSO4structure can have two forms, and it is shown that most previous data on the existence of the high temperatureα-CaSO4polymorphs are likely to be due to decomposition of the sulphate.Some observations on theγtoβ-CaSO4transformation are reported. The structural implications of these results and their relevance to the nature of the transformation are discussed.

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