它是中生代硅酸过饱和并富钾质的火山岩系的产物，其意义可与产于新生代碱性玄武岩系中的晶洞钠沸石对比。
It is a product of volcanic rocks of the mesozoic era over-saturated with silica and rich in potash. it can be compared with geode natrolite that producedin alkaline basalt series of the cenozoic era.
主要的成分有钾、钠、铝硅酸盐。
The main ingredients are potassium, sodium and aluminum silicate.
主要的成分有钾、钠、铝硅酸盐。
The main ingredients are potassium, sodium and aluminum silicate.
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