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Classification of the minerals of the graftonite group

机译:Graftonite组矿物的分类

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A classification and nomenclature scheme has been approved by the International Mineralogical Association Commission on New Minerals, Nomenclature and Classification for the minerals of the graftonite group. The crystal structures of these minerals have three distinct sites that are occupied by Fe2+, Mn2+ and Ca2+. These sites have coordination numbers [8], [5] and [6], and these differences lead to very strong order of Fe2+, Mn(2+ )and Ca2+ over these sites. As a result of this strong order, the following compositions have been identified as distinct species: graftonite: FeFe2(PO4)(2); graftonite-(Ca): CaFe2(PO4)(2); graftonite-(Mn): MnFe2(PO4 )(2); beusite: MnMn2 (PO4) (2); and beusite-(Ca): CaMn2(PO4)(2).
机译:国际矿物学协会委员会关于新矿物质,矿物质群体的矿物质,命名和分类批准分类和命名计划。 这些矿物的晶体结构具有三个不同的位点,其由Fe2 +,Mn2 +和Ca2 +占据。 这些位点具有协调数[8],[5]和[6],这些差异导致这些位点上的Fe2 +,Mn(2+)和Ca2 +的非常强烈的顺序。 由于这种强烈的顺序,已将以下组合物鉴定为不同的物种:Graftonite:FeFE2(PO4)(2); Graftonite-(CA):Cafe2(PO4)(2); Graftonite-(Mn):MnFe2(PO4)(2); 鸟冢:MNMN2(PO4)(2); 和鸟钻 - (CA):CAMN2(PO4)(2)。

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