摘要
该矿位于北武夷地区,矿床为酸性凝灰岩热液蚀变型叶蜡石矿床。文章论述了成矿地质特征以及控矿因素。
The deposit is located in North Wuyi area and is an acid tuff hydrothermal altered pyrophyllite deposit.The geological characteristics and ore-controlling factors were discussed in this paper.
作者
吴斌
吴欢军
Wu Bin;Wu Huanjun(Jiangxi Geological and Mineral Exploration and Development Bureau Northeast Jiangxi Brigade,Shangrao 334000,China)
出处
《有色金属设计》
2018年第4期1-3,共3页
Nonferrous Metals Design
关键词
地质特征
成因探讨
高岭石
Geological characteristics
Genesis discussion
Kaolinite
