Abstract
THE structure of the aluminosilicate frame of erionite was proposed and tested by Staples and Gard1. Hey and Fejer2 have stated that X-ray powder photographs of offretite from Mt. Simiouse, Montbrison, Loire, France3,4, were identical with those of erionite from Durkee, Oregon5,6. They claim that the name offretite has priority over erionite.
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References
Staples, L. W., and Gard, J. A., Min. Mag., 32, 261 (1959).
Hey, M. H., and Fejer, E. E., Min. Mag., 33, 66 (1962).
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Breck, D. W., and Acara, N. A., U.S. Patent No. 2,950, 952 (1960).
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O'Daniell, H., and Fischer, K., Amer. Mineralogist, 43, 175 (1958) (Abstract).
Fischer, K., Fortsch. Mineral., 38, 201 (1960).
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Bennett, J. M., thesis, Univ. Aberdeen (1966).
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BENNETT, J., GARD, J. Non-identity of the Zeolites Erionite and Offretite. Nature 214, 1005–1006 (1967). https://doi.org/10.1038/2141005a0
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DOI: https://doi.org/10.1038/2141005a0
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