甘肃省卓尼县窑沟铅矿床成因及成矿物质来源探讨  

Discussion on the Source of Ore Genesis of Yaogou Lead Deposit in Gansu Zhuoni

作　　者：谢平军[1] 

机构地区：[1]甘肃有色地质勘查局三队,甘肃白银730900

出　　处：《甘肃冶金》2011年第2期92-94,98,共4页Gansu Metallurgy

摘　　要：窑沟铅矿床位于祁吕狐西翼双朋喜-新堡复背斜南翼东段,其成矿与地层、构造、岩浆活动具有一定的联系。本文通过研究本区大地构造背景、成矿地质特征,初步分析了窑沟铅矿床的成矿期次、成矿物质来源,探讨了矿床成因,指出了找矿标志。Yaogou lead deposit,is located in the south wing of Shuangpengxi-Xinbu anticlinorium of Qiluhu west wing,its mineralization is connected with the stratum,construction and magma activities.This paper Studies the tectonic setting and geological features,preliminary analyze division of the mineralization periods,ore origin genesis and prospecting signs.

关 键 词：成矿物质来源 成矿期次 矿床成因 窑沟 

分 类 号：P611[天文地球—矿床学] P618.42[天文地球—地质学]