摘要
本文以地下水成矿理论，探讨了会理红盆南部爱国─湾子村砂岩型铜银矿点的成矿有利条件，根据构造对该类矿床的控制作用和金属矿物分带形成机制等新认识，阐明该区砂岩型铜矿床的控矿因素．
Based on the mineralization theory of underground water,this paper approaches the favourable mineral conditions of sandstone silver-copper mineral points at the Aiguo-Wanzicun in the Huili Red Basin.By contrasting the controlling functions of this kind of mineral,the controlling mineral factors in this region are expounded according to the new knowledge of the forming structures of metal mineral zoning
基金
国家自然科学基金
关键词
铜矿床
控矿因素
砂岩型
金属矿物
Sandstone copper-silver deposit,confluence basin,metal mineral zoning
