湘中锡矿山锑矿床围岩蚀变特征和矿化的关系  

Relations between Wall-rock Altered characteristics and Mineralization of Xikuangshan Sb deposit in Central Hu'nan

作　　者：于水 肖亮明 

机构地区：[1]锡矿山闪星锑业有限责任公司,湖南冷水江417502

出　　处：《铜业工程》2010年第1期38-42,共5页Copper Engineering

摘　　要：湘中锡矿山锑矿床是典型的中低温热液型矿床,矿区围岩蚀变发育,类型有硅化、方解石化、黄铁矿化、重晶石化、绢云母化等,并在矿区形成三个较清晰的围岩蚀变带。围岩蚀变与锑矿化的关系密切,对寻找锑矿床具有重要的意义。The Xikuangshan Sb deposit is a kind of medium - low hydrothermal deposit, with developed alteration of country rock in the mine area. The deposit is classified as types of silicification, caleitization, pyritization, baritization and sericitization etc. , three country rock alteration zones are obviously formed, which has a close relation with Sb mineralization and is very meaningful for prospecting Sb deposit.

关 键 词：锑矿床 围岩蚀变 矿化 

分 类 号：P5[天文地球—地质学]