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A heulandite with excess water
Published online by Cambridge University Press: 14 March 2018
Summary
A heulandite from Nelson Creek, Skamania County, Washington, has 30 H2O per unit cell instead of the normal 24; the excess water is lost on gentle heating. The b and c cell-dimensions are also rather larger than normal. Normal heulandite also occurs in the same area.
- Type
- Research Article
- Information
- Mineralogical magazine and journal of the Mineralogical Society , Volume 36 , Issue 277 , March 1967 , pp. 64 - 69
- Copyright
- Copyright © The Mineralogical Society of Great Britain and Ireland 1967
References
Deer, (W. A.), Howie, (R. A.), and Zussman, (J.), 1963. Rock-forming minerals, vol. 4. Framework silicates. London
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