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Sedimentary analcime at Murrurundi, New South Wales, Australia

Published online by Cambridge University Press:  05 July 2018

Beryl Nashar
Beryl Nashar*
Affiliation:
Department of Geology, The University of Newcastle, 2308, Australia
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Summary

Sedimentary analcime in a small basin in Cainozoic basalt at Murrurundi, New South Wales, has probably resulted from the reaction of Na-rich water on colloidal nontronite derived from volcanic ash. Based on cell dimension (13.713 Å) and Δ2θ(1·81) determined by Saha's (1959) method it is a Group C low-silica type of Coombs and Whetten (1967).

Type
Research Article
Information
Mineralogical Magazine , Volume 42 , Issue 322 , June 1978 , pp. 241 - 243
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1978

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References

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