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Fuller's earth from near Dry Branch., Georgia, a montmorillonite-cristobalite clay

Published online by Cambridge University Press:  02 May 2018

G. W. Brindley*
Affiliation:
Department of Ceramic Technology, The Pennsylvania State University, University Park, Pennsylvania
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Abstract

Fuller's earth from near Dry Branch, Georgia, is shown by X-ray analysis to contain comparable amounts of montmorillonite and cristobalite, and only minor amounts of other minerals. The cristobalite resembles the high form, but may be a very disordered low form. Electron micrographs show the montmorillonite to be lath-like, and the cristobalite globular in form.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1957

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References

Buerger, M. J. 1951. Phase Transformations in Solids, John Wiley & Sons, Inc., New York. (P.207–8).Google Scholar
Flörke, O. W. 1955a. Neues Jb. Miner. Mh., 217224.Google Scholar
Flörke, O. W. 1955b. Ber. dtsch. keram. Ges., 32, 369–81.Google Scholar
Gruner, J. W. 1940a. Econ. Geol., 35, 867–75.Google Scholar
Gruner, J. W. 1940b. Amer. Min., 25, 587–90.Google Scholar
Jagodzinski, H. and Laves, F. 1948. Schweiz. min. petrogr. Mitt., 28, 456–67.Google Scholar
Kesler, T. L. 1956. Econ. Geol., 51, 541–54.Google Scholar
Levin, I. and Ott, E. 1933. Zeit. Krist., 85, 305–18.Google Scholar