| 广西平南县苏屋金矿床地质特征及地球化学特征研究 |
| |
| 引用本文： | 黄赤新,王传建,冯玉君,王功民.广西平南县苏屋金矿床地质特征及地球化学特征研究[J].矿产与地质,2016(1):12-18. |
| |
| 作者姓名： | 黄赤新 王传建 冯玉君 王功民 |
| |
| 作者单位： | 广西第六地质队,广西 贵港,537100 |
| |
| 基金项目： | 广西地矿局2012年度部门预算前期工作项目((桂地矿科[2012]32号)资助。) |
| |
| 摘 要： | 广西平南县苏屋金矿床位于桂东大瑶山金多金属成矿带中部六岑金矿田内,矿体主要赋存在NE向断层破碎带中,次为近EW向与NW向,矿体走向、规模、延深,厚度及品位严格受断裂控制,矿体与围岩界线明显,矿石主要为硅化压碎岩,属中低温热液断裂充填型脉状矿床。
|
| 关 键 词： | 金矿床 地质特征 地球化学特征 找矿前景 |
Geological and geochemical characteristics of Suwu gold deposit in Pingnan of Guangxi |
| |
| Abstract: | Suwu gold deposit in Pingnan of Guangxi is located inside Liucen gold ore field of central Dayaoshan gold polymetallic metallogenic belt in eastern Guangxi.The orebodies occur predominantly in the NE-trending fault fracture zone,and subordinately in nearly EW and NW trends.The strike,scale,depth,thickness and grade of the orebodies are strictly controlled by faults and fractures,and the boundary line between orebody and wall rock is clear.The ores are mainly siliceous crushed rocks.The deposit is a mid-low temperature hydrothermal fracture filling type vein deposit. |
| |
| Keywords: | gold deposit geological characteristic geochemical characteristic prospecting potential |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
|
