湖南新晃上关溪—高寨硒汞矿地质特征及找矿意义  

Geological Feature of Shangguanqi-Gaozai Se-Hg Deposit in Xinhuang of Hunan and Its Significance of Seeking for the deposit

作　　者：包正湘 万溶江 鲍觉敏 

机构地区：[1]湖南湘西地勘5队,湖南吉首416007

出　　处：《贵州地质》1999年第4期321-324,共4页Guizhou Geology

摘　　要：湖南新晃上关溪—高寨硒汞矿严格受构造控制,产于硅化岩(微石英岩)内。研究表明,该区高寨地段具有硒汞矿找矿远景,区内的富硒地球化学场,可开展“汞中找金”工作。Shangguanqi-Gaozai Se-Hg deposit in Xinhua of Hunnan is under strict control of the structure ,and occurs in the silicified rock,that is micro-quartzite.The study shows that there exists the forecast on seeking for the selenium-mercury deposit of Gaozai block in this region.Within the regional geochemical field of enrich selenium,the researcher can develop the works in the exploration of gold from mercury deposit.Since the author firstly discovered upper Guanqi selenium and mercury deposit in Xinhuang of Hunan in seventies century,the study on seeking for the selenium on the belt of Xiang-Qian mercury deposit make great progress.On the basis of the above geological feature of this region,the paper discusses the forecast and significance of seeking for the selenium and mercury deposit.

关 键 词：硒汞矿 地质特征 找矿意义 汞矿 

分 类 号：P618.680.2[天文地球—矿床学] P618.680.8[天文地球—地质学]