贵州雷公山地区摆吉锑矿矿床成因探讨  

A Preliminary Analysis on Genesis of Baiji Antimony Ores Deposit, Leigongshan, Guizhou

作　　者：陈永科[1] 李坤[1] 游连强[1] 

机构地区：[1]贵州省地矿局地质大队,贵州都匀558000

出　　处：《贵州地质》2004年第1期41-47,共7页Guizhou Geology

摘　　要：　本文阐述了贵州雷公山地区摆吉锑矿成矿地质背景、矿床地质特征,对成矿条件、成矿机理进行了分析,对矿床的成因进行了探讨,认为矿床属受剪切带控制的幔源中低温热液矿床。Geological setting of metallogenetic and geological feature of Baiji antimony ores deposit are expounded, studies of ore-forming conditions and mechanism and the genesis of the deposit are conducted, it is proposed that this deposit is a mantle-derived low-middle temperature hydrothermal deposit dominated by the shearing zone.

关 键 词：锑矿 矿床成因 过渡性剪切带 断层破碎带 构造运动 

分 类 号：P618.66[天文地球—矿床学] P611[天文地球—地质学]