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Ephesite : ウィキペディア英語版
Ephesite

Ephesite is a rare member of the mica silicate mineral group, phyllosilicate. It is restricted to quartz-free, alumina rich mineral assemblages and has been found in South African deposits in the Postmasburg district as well as Ephesus, Turkey.〔Phillips, F. (1931) ''Ephesite (soda-maragrite) from the Postmasburg district, South Africa,''
Corpus Christi College, Cambridge, pp. 482-485〕
== Composition ==
Ephesite has an ideal chemical formula of NaLiAl2(Al2Si2)O10(OH)2.〔Rieder, M. et al. (1998) Nomenclature of the Micas. The Canadian Mineralogist, 36, 41-48〕 Ephesite and paragonite are closely related due to their substitution of sodium in place of potassium. The general form of most micas, which can vary such as in the place of ephesite, can be written as W(X,Y)2-3Z4O10(OH,F)2 as observed by many sources. In the case of ephesite the W compound is sodium and the (X,Y) is lithium and aluminium, it also bears two hydroxides as the end members.〔

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