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Note on the occurrence of anatase in some fireclay deposits

Published online by Cambridge University Press:  14 March 2018

G. W. Brindley  and
Keith Robinson
G. W. Brindley
Affiliation:
Physics Laboratories, University of Leeds
Keith Robinson
Affiliation:
Physics Laboratories, University of Leeds
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Extract

In X-ray studies of fireclays we have frequently observed the presence of anatase to the extent of 1 or 2% with little or no rutile, and no brookite. Chemical analyses of these clays usually record 1–2% of TiO2 and occasionally more (Ennos and Scott, 1924). The mineralogical form of the TiO2 is usually not stated, but a number of references to the observance of rutile needles give the impression that rutile is the form in which titania occurs in these deposits. Our own observations based on X-ray powder photographs lead us to conclude that anatase is commonly present and that rutile is either absent or present in smaller quantities. We have not detected brookite.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 28 , Issue 199 , December 1947 , pp. 244 - 247
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1947

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