摘要
根据同源岩浆演化的观点，运用岩石谱系单位的划分方法，将景宁花岗岩基解体，划分为９个单元，归并成２个超单元。岩体定位方式为断裂扩张型。
From the viewpoint of comagmatic evolution and using the method of lithodemic division, the Jingning granite batholith is divided into nine units, which are incorporated into two super units. The emplacement mechanism of the granites is of fracture propagation type.
出处
《中国区域地质》
CSCD
1998年第4期430-435,共6页
Regional Geology of China
关键词
景宁花岗岩基
单元
超单元
断裂扩张型
花岗岩
Zhejiang, Jingning granite batholith, unit, super unit, fracture propagation type
