A new interpretation of the structure of
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M. J. Wilson; J. D. Russell; J. M. Tait
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Article
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1974
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Springer
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English
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Disordered c~-cristobalite which occurs extensively in bentonites, opals and particularly deep-sea cherts, has been previously interpreted in terms of a nnidimensionally disordered structure in which cristobalite is interstratificd with two-layer tridymite-like sheets. An alternative interpretation