Hostname: page-component-78c5997874-dh8gc Total loading time: 0 Render date: 2024-11-14T13:26:10.493Z Has data issue: false hasContentIssue false

Vein-Like Sepiolite Occurrence As a Replacement of Magnesite in Konya, Turkey

Published online by Cambridge University Press:  02 April 2024

Mefail Yeniyol*
Affiliation:
Department of Geology, University of Istanbul, Istanbul, Turkey
Rights & Permissions [Opens in a new window]

Abstract

Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Note
Copyright
Copyright © 1986, The Clay Minerals Society

References

Bailey, S. W., Brindley, G. W. and Brown, G., 1980 Structures of layer silicates Clay Minerals and Their X-ray Identification London Mineralogical Society 1123.Google Scholar
Brauner, K. and Preisinger, A., 1956 Struktur und Enstehung des Sepioliths Tschermaks Min. Petr. Mitt. 6 120140.CrossRefGoogle Scholar
Brindley, G. W., Brindley, G. W. and Brown, G., 1980 Order-disorder in clay mineral structures Clay Minerals and Their X-ray Identification London Mineralogical Society 125195.Google Scholar
Caillère, S., Hénin, S. and Mackenzie, R. C., 1957 The sepiolite and palygorskite minerals The Differential Thermal Investigation of Clays London Mineralogical Society.Google Scholar
Grim, R. E., 1953 Clay Mineralogy New York McGraw-Hill.CrossRefGoogle Scholar
Nagata, H., Shimoda, S. and Sudo, T., 1974 On dehydration of bound water of sepiolite Clays & Clay Minerals 22 285293.CrossRefGoogle Scholar
Post, J. L., 1978 Sepiolite deposits ofthe Las Vegas, Nevada area Clays & Clay Minerals 26 5864.CrossRefGoogle Scholar
Rautureau, M. and Mifsud, A., 1977 Etude par microscope électronique des différents états d’hydration de la sépiolite Clay Miner. 12 309318.CrossRefGoogle Scholar
Serna, C., Ahlrichs, J. L. and Serratosa, J. M., 1975 Folding in sepiolite crystals Clays & Clay Minerals 23 452457.CrossRefGoogle Scholar
Siffert, B. and Wey, R., 1962 Synthèse d’une sépiolite à température ordinaire CR. Acad. Sci. Paris 254 14601462.Google Scholar