湖南新化锡矿山锑矿成因分析  

Genetic Analysis of Tin Mine Antimony Deposit in Xinhua, Hunan

作　　者：李玲 陈锌 LI Ling;CHEN Xin(Chengdu University of Technology, Chengdu 610059, China)

机构地区：[1]成都理工大学,四川成都610059

出　　处：《四川有色金属》2018年第4期22-24,共3页Sichuan Nonferrous Metals

摘　　要：湖南新化锡矿山(原属新化县)的锑矿储量庞大,前人曾做了大量的工作,探究其成因,为找矿提供依据。本文从化学元素的角度切入,主要通过分析矿区演变前后其化学成分的变化,推断出锡矿山锑矿的成矿原因为热液蚀变。The antimony deposits in Xinhua tin mine(formerly Xinhua County)in Hunan Province are huge.The predecessors have done a lot of work to explore their causes and provide a basis for prospecting.From the point of view of chemical elements,this paper deduces that hydrothermal alteration is the cause of antimony mineralization in tin mine by analyzing the changes of chemical composition before and after the evolution of the mining area.

关 键 词：锡矿山 锑矿成因 热液蚀变 

分 类 号：P618[天文地球—矿床学]