Solid solutions of offretite, direnzoite, and ferrierite


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Abstract

The three-dimensional geometric analysis carried out in this study has made it possible to clearly outline the homogeneity regions of solid solutions rich in magnesium and potassium oxides. Common elements in the structures of the zeolites (offretite, direnzoite, and ferrierite-Mg) have been identified and the factors responsible for the distinctions between their structures have been analyzed.

About the authors

T. N. Kol’tsova

Kurnakov Institute of General and Inorganic Chemistry

Author for correspondence.
Email: koltsova@igic.ras.ru
Russian Federation, Leninskii pr. 31, Moscow, 119991

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