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An occurrence of phlogopite and its transformation to vermiculite by weathering

Published online by Cambridge University Press:  14 March 2018

W. W. Smith Aitken
W. W. Smith Aitken*
Affiliation:
The Macaulay Institute for Soil Research, Aberdeen, Scotland
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Summary

The characteristics of a phlogopite and its weathering product, vermiculite, have been studied by X-ray, infra-red, electron-microscope, and chemical methods. Inclusions within these minerals have been identified as thin films rich in iron oxide (which impart a schiller effect), spinel (which may exist in a preferred orientation), and serpentine. The orientation relationship between the fresh mica and its weathering product has been established by single-crystal methods. The mechanism of transformation from a 1-layer to a 2-layer polytype is discussed.

Information

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 35 , Issue 269 , March 1965 , pp. 151 - 164
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1965

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References

Ball, (M. C.) and Taylor, (H. F. W.), 1961. Min. Nag., vol. 32, p. 754.Google Scholar
Barshad, (L.), 1954a. Soil Sci., vol. 77, p. 463.Google Scholar
Barshad, (L.), 1954b. Ibid., vol. 78, p. 57.Google Scholar
Brindley, (G. W.), Ouchton, (B. M.), and Robinson, (K.), 1950. Aeta Cryst., vol. 3, p. 408.Google Scholar
Brown, (B. E.) and Bailey, (S. W.), 1962. Amer. Min., vol. 47, p. 819.Google Scholar
Brown, (G.)(editor),1961. The X-ray identification of clay minerals. Mineralogical Society, London.Google Scholar
Gower, (J. A.), 1957. Amer. Journ. Sci., vol. 255, p. 142.Google Scholar
Gruner, (J. W.), 1934. Amer. Min., vol. 19, p. 557.Google Scholar
Hendricks, (S. B.) and Jefferson, (M. E.), 1938. Amer. Min., vol. 23, p. 851.Google Scholar
Hendricks, (S. B.) and Jefferson, (M. E.), 1939. Ibid., vol. 24, p. 729.Google Scholar
Judd, (J. W.), 1885. Quart. Journ. Geol. Soc., vol. 41, p. 401.Google Scholar
Lacroix, (A.), 1940. Compt. Rend. Acad. Sci. Paris, vol. 210, p. 353.Google Scholar
Levinson, (A. A.) and Heinrich (E. WM.), 1954. Amer. Min., vol. 39, p. 937 [M.A. 12-529].Google Scholar
Mathieson, (A. McL.) and Walker, (G. F.), 1954. Ibid., vol. 39, p. 231.Google Scholar
Phemister, (J.), 1960. Brit. Reg. Geol. Scotland: The Northern Highlands, p. 61. Edinburgh, H.M.S.O.Google Scholar
Smith, (J. V.) and Yoder, (H. S.), 1956. Min. Mag., vol. 31, p. 209.Google Scholar
Steinfink, (H.), 1962. Amer. Min., vol. 47, p. 886.Google Scholar
Walker, (G. F.), 1949. Min. Mag., vol. 28, p. 693.Google Scholar
Weaver, (C. E.), 1958. Amer. Min., vol. 43, p. 839.Google Scholar