摘要
论述了嵩溪银-锑矿床地质特征、矿化富集规律,并通过对矿床的构造环境、矿石结构构造、成矿物理化学条件等的分析,得出矿床成因为火山喷流沉积-热液改造型矿床的结论。
The paper discusses geological characters and metallogeny of the Songxi silver and antimony deposit and analyzes the structure environment, ore texture and ore forming physical and chemical conditions. It is concluded that the genesis of the deposit belongs to volcanic spout deposition-hydrothermal transformed deposit.
出处
《矿产与地质》
2005年第4期375-379,共5页
Mineral Resources and Geology
关键词
银-锑矿床
成因
地质特征
嵩溪
粤东
silver and antimony deposit
genesis
geological character
songxi
east Guangdong
