摘要
淅川银、锑、钒多金属矿带是通过1:5万水系沉积物测量、异常检查而后开展矿产评价工作而发现的,赋矿岩石为寒武系底部水沟口组的硅质岩和粘土岩。多金属带以银、锑、钒矿化为主,伴有金、铂钯、稀土等矿化,是在滨-浅海沉积环境中并经后期构造热液活动形成,区域上存在众多的相同相近地质地球化学背景,区域矿产有一定潜力。
The Xichuan Ag, Sb, V multimetal ore zone was found in 1:50000 water system sediment survey, abnormity check and mineral resources evaluation. The zone hosted in siliceous and clay rock of Shuigoukou formation at the bottom of Cambrian. The multimetal ore zone is dominated by Ag,Sb,V and associated with Au, Pt, Pd and REE mineralization. The zone was reformed by tectonic hydro-thermal activity in littoral - shallow sea with a lot of the same geochemical background as the other regions.
出处
《资源调查与环境》
2005年第1期43-48,共6页
Resources Survey & Environment
基金
国土资源大调查项目(编号:0499141055)资助
