赣南钨矿床断裂构造地球化学研究意义简析  

On the Fracture Structure Geochemistry of Tungsten Deposits in Southern Jiangxi

作　　者：吴开兴[1] 朱忠[1] 何书[1] 

机构地区：[1]江西理工大学资源与环境工程学院,江西赣州341000

出　　处：《中国钨业》2009年第3期7-10,共4页China Tungsten Industry

摘　　要：构造地球化学是构造成矿动力学及隐伏矿定位预测的重要研究内容,已在隐伏矿预测方面取得显著进展,但尚未在赣南钨矿区系统开展。笔者分析了开展赣南钨矿床断裂构造地球化学研究的现实必要性。Being an important part of the study of dynamics of tectonic ore-forming process and localization- prognosis of concealed ore bodies, fracture structure geochemistry research has already made a great progress. However, fracture structure geochemistry has still not been systematically applied in tungsten deposits in southern Jiangxi. This paper discusses the practical necessity and significance of launching fracture structure geochemistry research in tungsten deposits in southern Jiangxi.

关 键 词：赣南 钨矿床 断裂构造地球化学 

分 类 号：P618.67[天文地球—矿床学]