Paragonite
- 网络钠云母

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The Na + ions released from the alteration of the sodic ash made the kaolinite transform into paragonite , forming the special mineral assemblage in both of them .
在蚀变过程中析出的部分Na+离子,促使高岭石向钠云母转化,形成了高岭石加钠云母的特殊组合。
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The mineral assemblages in the main stage are garnet + phengite + quartz + magnetite ± paragonite ± epidote / zoisite in the mica schist ;
主期阶段的矿物组合在云母片岩中为石榴石+多硅白云母+石英+磁铁矿±钠云母±绿帘石/黝帘石;