n.閃巖

They belong to the amphibolite facies. 屬于角閃巖相產(chǎn)物。

The formation the LILE-rich amphibolite is resulted from the LILE-rich hydrothermal fluid emplacement, which provide the material source for the Kuerti plagiogranite formation. 由于受富含輕稀土等大離子親石元素的熱水流體的交代，形成了富集大離子親石元素的角閃巖。

斜長角閃巖