云南白牛厂超大型银多金属矿床黄铁矿的标型特征及其成因意义  

THE TYPOMORPHIC CHARACTERISTIC OF PYRITES AND ITS GENETIC MEANING IN BAINIUCHANG SIL VER-POLYMETALLIC DEPOSIT, YUNNAN PROVINCE

作　　者：白金刚[1] 池三川[1] 梅建明[1] 

机构地区：[1]中国地质大学

出　　处：《贵金属地质》1995年第4期302-306,共5页

摘　　要：本文通过对白牛厂银多金属矿床黄铁矿的化学成分标型、微量元素标型和热电性标型的研究得出该矿床属热液喷流沉积矿床。In this paper，the authors have studied the typomorphic characteristic of pyrites in de-tails，such as Chemical Composition and thermoelectric structures of pyrites.From the study，we can come to this Conclusion：the Bainiuchang Silver-polymetalhic deposit is a Sedimenta-ry deposit of exhalation.

关 键 词：银矿床 多金属矿床 黄铁矿 标型特征 成因 

分 类 号：P618.520.4[天文地球—矿床学] P618.204[天文地球—地质学]