摘要
通过对深部隐伏花斑岩体群的研究，首次确认黄沙坪矿田中铜矿床的存在，花斑岩是铜矿床的成矿母岩，矿体产出形式受围岩条件、构造部位的控制，构成“四位一体”的复式成矿。
The exist of copper deposit is first affirmed in Huangshaping ore field through researching the deep blind granite porphyry group,the granite-prophyry is the matallogenic matrix of copper deposit.Occrurance of copper orebody is controlled by wallrock conditions and structure position,it is a complex metallogeny deposit of the difference kind styles existing together.
出处
《湖南地质》
1999年第2期75-78,共4页
Hunan Geology
