湖南铲子坪金矿床地质特征及找矿标志  

On geological characteristics and ore prospecting indicators of Chanziping gold deposit in Hunan

作　　者：曹有金[1,2] 李剑[3] 陈锋 汪长江 刘邦定[1] 

机构地区：[1]湖南科技大学土木工程学院,湖南湘潭411201 [2]页岩气资源利用湖南省重点实验室,湖南湘潭411201 [3]湖南省国土资源规划院,湖南长沙410007 [4]湖南省407地质队,湖南怀化418000

出　　处：《地质学刊》2014年第2期309-313,共5页Journal of Geology

基　　金：国家自然科学基金(40902062);湖南省教育厅优秀青年项目(12B039)资助

摘　　要：铲子坪金矿位于雪峰弧形构造带中段,是湖南省发现最早的破碎带蚀变岩型金矿床。通过对金矿床地质特征的综合分析,总结出该矿床的找矿标志,对该区进一步找矿预测有指导意义。Chanziping gold deposit was located in the middle of Xuefeng arc tectonic belt in Hunan Province,and was the earliest altered cataclastic altered rock type gold deposit. Through a comprehensive analysis of the geological features of gold deposit,the authors summarized the prospecting indicators,and was of important significance for further prospecting prediction in the study area.

关 键 词：地质特征 找矿标志 铲子坪金矿 湖南 

分 类 号：P618.51[天文地球—矿床学]