正 本文所研究的钠沸石(Natrolite)晶体产于安徽当涂釜山和江苏六合塔山的玄武岩晶洞中。钠沸石是发现最早(1758)的沸石族矿物之一,一些学者对它做了不少矿物学方面的...
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与钠沸石、层硅铈钛矿、钙霞石等伴生。
Wadeite is paragenic with aegirine, nepheline, arfredsonite, microcline and apatite, and associated with natrolite, rinkite and cancrinite.
还用负离子配位多面体生长基元理论模型分析解释了钠沸石的合成机理。
The forming mechanism of natrolite has been illustrated by electronegative ion polyhedron of coordination growths unit theoretical model.
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.
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