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.
花岗伟晶岩一种有时富含铀、钨和钽等稀有元素的粗纹理花岗岩。
A coarse-grained granite, sometimes rich in rare elements such as uranium, tungsten, and tantalum.
其中辉绿岩和煌斑岩是典型的幔源岩，花岗伟晶岩则是典型的壳源岩。
The diabase and lamprophyre are typical mantle source rock while the granite pegmatite is typical crustal source rock.
出露地层为震旦系、泥盆系、二叠系、三叠系以及侵入的花岗岩脉和花岗伟晶岩脉。
Emergence stratums are of Sinian, Devonian, Permian, Trias and intrusive granite dike and coarse - grained granite dike.
地球化学和同位素研究表明，该矿床为岩浆一交代花岗伟晶岩型矿床，成因上与付坊和会同岩体有关。
The research on geochemical characteristics and isotope age suggests that the deposit belongs to a magma-metasomatic pegmatite type deposit related to Fufang and Huitong granitic mass in genesis.
新疆阿尔泰地区某些花岗伟晶岩含有金绿宝石，它是一种罕见的稀有元素矿物，而且具有极高的经济价值。
Chrysoberyl in some granite pegmatite is a rare mineral that seldom seen in Altatic area, and it is a valuable precious stone.
东湖伟晶岩矿床为花岗质完全分异式伟晶岩类型；
Donghu pegmatite deposit is characterized by granitic and completely differential pegmatite.
东湖伟晶岩矿床为花岗质完全分异式伟晶岩类型；
Donghu pegmatite deposit is characterized by granitic and completely differential pegmatite.
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