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1989年,作者在我国湖北省郧阳地区寒武系黑色岩系中发现了一种含钒、钾、钒元素为待征的层状具有附加阴离子的铝硅酸盐新矿物。矿物中K、Ba两元素并重,分别在晶体结构中占独立的结晶学位置。晶体结构特点是K、Ba沿b轴方向有序化分布,可以看成云母族与黄绿脆云母族的矿物晶体结构沿b轴加和,使b_0加上一倍。根据矿物分类原则可以建立新矿物族一中华云母族,并将该族第一个代表性的新矿物命名为“中华云母”(Zhong huanite)。
In 1989, the authors discovered a new aluminosilicate mineral with additional anions in the Cambrian black rock series of Yunyang area in Hubei Province, China, which contains vanadium, potassium and vanadium elements. Minerals K, Ba two elements, respectively, in the crystal structure occupies an independent crystallographic position. Crystal structure is characterized by K, Ba ordered along the b-axis direction of the distribution can be seen as mica and yellow-green brittle mica mineral crystal structure along the b-axis sum, b_0 doubled. According to the principle of mineral classification, a new mineral family-Chinese mica can be established, and the first representative new mineral of this group is named “Zhong huanite”.