摘要
沃溪矿床深部隐伏矿体是近几年发现的新矿体,构造的多级控矿作用十分明显,矿体受边幕式排列的隐伏层间断层和隐伏层间褶皱控制,赋矿岩性为元古宇板溪群马底驿组紫红色绢云母板岩。隐伏矿体的发现不仅为矿山增加了储量,而且为研究区进一步勘查隐伏矿体开辟了新途径。
The buried ore body in the depths of Woxi deposit is a new one found in the recent years.It appears very distinctly multi grade ore control role of structure and is controlled by enechelon faults and folds of buried inter layer.The ore yielding stratum is purple sericite slate of Madiyi formation,Banxi group,Pt.The discovery of the buried ore body has not only increased the reserves but also opened up a new path for the deep exploration of the buried ore body in this region。
出处
《黄金地质》
1998年第3期35-39,共5页
Gold Geology
关键词
金锑钨矿
隐伏矿体
地质特征
控矿构造
共生矿床
W Sb Au deposit, blind ore body, geologic feature, ore control structure, Hunan