| 1. | Pegmatites seem to form during a late magmatic stage .
伟晶岩似乎是在较晚的岩浆阶段形成的。 |
| 2. | At pegmatite contacts the composition changes to chalcopyrite, millerite, pyrite, and violarite accompanied by magnetite and hematite .
在伟晶岩接触带，硫化物成分变为黄铜矿、针镍矿、黄铁矿及硫镍铁矿，伴生有磁铁矿和赤铁矿。 |
| 3. | Corundum oligoclase pegmatite
刚玉奥长伟晶岩 |
| 4. | Epidote oligoclase pegmatite
绿帘奥长伟晶岩 |
| 5. | Epidote orthoclase pegmatite
绿帘正长伟晶岩 |
| 6. | Elaeolite - syenite - pegmatite
脂光正长伟晶岩 |
| 7. | Epidote albite pegmatite
绿帘钠长伟晶岩 |
| 8. | Purple fluorite is a stone of intuition and aids in seeing to the core of matters
无色透明的萤石晶体产于花岗伟晶岩或萤石脉的晶洞中。 |
| 9. | A coarse - grained granite , sometimes rich in rare elements such as uranium , tungsten , and tantalum
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 |
| 10. | The pegmatite nb - ta mineral veins were controlled by a group of horizontal tenso - shear axial - direction fault - fissure systems in the nne direction folding structures
铌钽伟晶岩矿脉受控于nne向褶皱构造的一组近水平张扭性轴向裂隙系。 |
