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Publikováno v:
Mineralogical Magazine and Journal of the Mineralogical Society. 25:212-216
The structures of the fibrous zeolites edingtonite, thomsonite, and natrolite (with scolecite and mesolite) were determined by X-ray methods some years ago, and it was suggested shortly afterwards by M. H. Hey and F. A. Bannister in a private communi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0750852f264ad94b693ffe9c9ae96e60
https://doi.org/10.1180/minmag.1938.025.163.04
https://doi.org/10.1180/minmag.1938.025.163.04
