An X-ray examination of mordenite (ptilolite)
Published online by Cambridge University Press: 14 March 2018
Extract
The structures of the fibrous zeolites edingtonite, thomsonite, and natrolite (with scolecite and mesolite) were determined by X-ray methods some years ago, and it was suggested shortly afterwards by M. H. Hey and F. A. Bannister in a private communication to one of us (W.H.T.) that ‘ptilolite’, another zeolite of fibrous habit, might prove to have a similar structure. An X-ray rotation photograph about the needle axis indicated a unit-cell dimension along the needle axis of approximately 7·5 Å., quite different from the axis c 6·6 Å. characteristic of the fibrous zeolites previously examined, and no further examination of ‘ptilolite’ was made at that time. We have now determined the unit cell and space-group of this crystal, and further work is in progress with a view to the complete analysis of the structure. This paper presents an account of the experimental data which we have obtained.
- Type
- Research Article
- Information
- Mineralogical magazine and journal of the Mineralogical Society , Volume 25 , Issue 163 , December 1938 , pp. 212 - 216
- Copyright
- Copyright © The Mineralogical Society of Great Britain and Ireland 1938
References
- 2
- Cited by