摘要
分析了四川省巴塘县夏塞银铅锌矿床区域成矿地质背景和控矿地质特征 ,指出区内NW向构造为导矿构造 ,矿体的产出严格受NNW向平行断裂系统控制。研究结果表明 ,富矿体在NNW向断裂中按一定间距连续出现 ,并在NNW向断裂伴生的次级构造中集中产出。
A study of regional geological setting and ore-control factors for the Xiasai Ag-Pb-Zn deposit indicates that NW-trending structures act as conduits for ore fluids and orebodies are controlled by a NNw-trending fault system, while ore shoots are confined equidistantly to secondary structures associated with the NNW-trending fault system.
出处
《四川地质学报》
2002年第4期201-204,共4页
Acta Geologica Sichuan