矿石类型为褐铁矿化破碎硅化砂岩、石英细脉和层状复理石韵律矿石。
Ore types are limonite fractured silicic sandstone, quartz veinlet and bedded flysch rhythm ore.
蚀变是区内的找矿标志之一,金矿的形成与硅化、褐铁矿化、黄铁矿化等蚀变有关。
The development of gold deposit in this area is connected with alteration, such as silicification, ferritization, pyritization.
前言:本文围绕与微细浸染型金矿有关的硅化、 褐铁矿化、 粘土矿化、 碳酸盐化等蚀变标志,在黔桂地区进行了相关的地球化学和光谱信息研究。
This paper studies the geochemical and spectral information on the"silification". "lemonitization". "clayization". and "carbonatization"related to finedesseminated-type gold deposits in Qian Gui area.
前言:本文围绕与微细浸染型金矿有关的硅化、 褐铁矿化、 粘土矿化、 碳酸盐化等蚀变标志,在黔桂地区进行了相关的地球化学和光谱信息研究。
This paper studies the geochemical and spectral information on the"silification". "lemonitization". "clayization". and "carbonatization"related to finedesseminated-type gold deposits in Qian Gui area.
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