云南泸水自把铅矿矿床地质及成因  

THE GEOLOGY AND GENESIS OF ZIBA PB DEPOSIT OF LUSHUI,YUNNAN

作　　者：肖祥春[1] 陶云花[1] 

机构地区：[1]云南黄金矿业集团股份有限公司,云南昆明650215

出　　处：《云南地质》2012年第2期200-203,199,共5页Yunnan Geology

摘　　要：矿床受地层及断层双重控制,走向长大于3千米,共圈出V1、V2、V3三条矿体。含矿岩石以透辉石矽卡岩为主,矿石工业类型为硫化铅矿石和氧化铅矿石。矿床成因类型为与花岗岩有关的含矿热液沿破碎带充填-交代形成的矽卡岩型铅矿床。The ore deposit is controlled by the bed and fault,strike NW,dip NE,length more than 3000m.There are 3 ore bodies,V1,V2,V3.The main ore-bearing rock is the dioside skarn.The commercial ores are Pb sulfide and Pb oxide.It belongs to the Pb deposit of skarn type,which is formed by the filling and metasomatism of thermal fluid related with the granite.

关 键 词：矽卡岩型铅矿 热液充填交伏 断层破碎带 与花岗岩有关 云南泸水自把 

分 类 号：P618[天文地球—矿床学]