摘要
维西县山加铜矿矿体呈透镜状、脉状沿构造破碎带产出,构造破碎带控矿明显,矿石矿物为孔雀石、蓝铜矿、辉铜矿、黄铜矿。为多期富集成矿特点,为中低温热液充填(交代)型铜多金属矿床。
The orebody of Shanjia Cu deposit in Weixi is lenticular,veined along structural fracture zone,which is controlled clear by the structural fracture zone.The ore minerals are malachite,azurite,cyprite,chalcopyrite,with the multiphase concentration metallogenesis feature.It is a middle-low T hydrothermal filling(metasomatism)Cu multimetallic deposit.
作者
李超
LI Chao(Wenshan Dounan Mn Mining Company(Ltd)of Yunnan,Wenshan 653000)
出处
《云南地质》
2018年第1期37-40,共4页
Yunnan Geology
关键词
构造破碎带控矿
热液型矿床
云南维西山加
Ore Control of Structural Fracture Zone
Hydrothermal Deposit
Shanjia,Weixi,Yunnan
