摘要
湖南省界牌钨铜多金属矿床位于雪峰山弧形构造带南段东缘加里东褶皱带与南岭东西向构造带北缘交汇部位的铺里—界牌断裂西侧,成矿条件优越。矿体产于寒武系上统(∈3)与岩体的内外接触带,NNE向断裂(F1)为导矿构造,地层与岩体的接触带、层间构造带是有利的成矿部位,矿化以钨矿化为主,次为铜矿化,为典型矽卡岩型钨铜矿床。
The Jiepai W-Cu deposit in Xinning,Hunan lies on the western side of the Puli-Jiepai fracture zone in the intersection of the Xuefengshan arc structure and the Nanling structure zone.The deposit is a typical skarn type W-Cu one and confined to the contact zone of the Upper Cambrian and an intrusion with NNE-trending fracture as passage-way for ore fluids.
出处
《四川地质学报》
2011年第2期153-156,共4页
Acta Geologica Sichuan
关键词
钨铜矿床
地质特征
控矿因素
界牌
W-Cu deposit
geological feature
ore control factor
Jiepai
