锂辉石为典型的伟晶岩矿物，主要生成于花岗伟晶岩脉中。

Spodumene is a typical kind of pegmatite, which forms mainly in the ore vein of granite-pegmatite.

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此外，还有矿物组合与辉长岩相似的辉长伟晶岩；与霞石正长石相似的霞石正长伟晶岩等等。

In addition, mineral assemblage and gabbro similar to gabbro pegmatite; and nepheline syenite nepheline syenite rock similar pegmatite and so on.

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霞石为典型的碱性矿物，主要生成于碱性岩及其伟晶岩中。

Nepheline is a typical kind of alkaline mineral, which forms mainly in alkaline deposit and its pegmatite.

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