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Rhythmic Banding of Ferric Oxide in Silicified Rhyolite Tuffs.1

Published online by Cambridge University Press:  01 May 2009

H. L. Chhibber
H. L. Chhibber
Affiliation:
Department of Geology and Geography, University College, University of Rangoon.
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Extract

A case is described of rhythmic banding by iron oxide in a rhyolitic tuff. The fine-grained tuff has acted as a medium for the production of Liesegang rings, the irregularity in the rings being ascribed to minute variations in the texture of the rock, naturally less homogeneous than a gel.

Type
Original Articles
Information
Geological Magazine , Volume 64 , Issue 1 , January 1927 , pp. 7 - 10
Copyright
Copyright © Cambridge University Press 1927

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Footnotes

1

Read at the Indian Science Congress, Bombay, 1926, vide Abstracts of Papers

References

page 7 note 2 Tarr, W. A., ‘Rhythmic Banding of Manganese dioxide in Rhyolite Tuff,’ Journ. Geology, vol. xxvi, 1918, pp. 610–17.CrossRefGoogle Scholar

page 7 note 3 Op. cit.

page 9 note 1 Holmes, H. N., ‘Rhythmic Banding’: Science, new series, vol. xlvi, 1917, 422.Google Scholar

page 9 note 2 Stamp, L. D., and Chhibber, H. L., Trans. Min. and Geol. Inst. India, vol. xx, 1925.Google Scholar