浅色花岗岩

浅色花岗岩脉BH-2-3的稀土元素配分模式和所有分析的样品都不一样，推断BH-2-3有可能是古老变质岩部分熔融的产物。

The REE distribution pattern of BH-2-3 differs however from the patterns of all the other samples . The major and rare earth element geochemistry of BH-2-3 suggests that it was derived from partial melting of ancient metamorphic rocks .

西武夷地区早古生代浅色花岗岩的厘定及其造山意义

Identification of the early Palaeozoic leucocratic granite in the West Wuyi Mountain Area and its orogenic implication

以上数据和与本区处在同一构造单元的前苏联矿区阿尔泰及山区阿尔泰12个浅色花岗岩结石U－Pb年龄180－200Ma的结果一致；

These age data are consistent with those ( Zircon U-Pb ages , 180 - 200Ma ) of the leucocratic granites from the Mining Altai and Mountainous Altai of the former Soviet Union , which are located in the same tectonic unit as the studied region .