摘要
桂阳大溪岭锑矿６号主矿脉受断裂控制明显，矿体主要赋存子断裂走向５°－２０°方向区段及倾角８０°～８８°的陡立部位。其资源量约占全矿区锑总资源量的６０％．
The No.6 vein of Daxiling antimony deposit is obviously controlled by the change of the fracture. The ore body mainly hosted in the fracture along the strike from NNE 5-20 and in the dip angle 80-88. Its reserves accounted up 60 percent of the antimony resource in this area.
出处
《湖南地质》
2001年第1期25-28,共4页
Hunan Geology
基金
国土资源大调查项目!(项目编号: 19991020070003)"大溪岭矿区锑矿评价"成果之一。
关键词
断裂控矿
锑矿床
矿床地质
控矿作用
找矿方向
Mineralization controlled by fracture
The major vein of No.6
Antinony deposit
