摘要
金矿体明显受断裂构造及石英脉体的双重控制。根据矿床地质特征分析,认为该矿床成因为沿构造劈理充填、改造的中低温低硫热液石英含金硫化物复合脉型矿床,具中—大型远景规模。
The Au orebody is evidently controlled by both fault and quartz vein. According to the analysis of geological characteristics, we believe that this ore deposit belongs to the reformed middle - low T hydrothermal deposit of quartz and Au - bearing sulfid composite vein （ filling along structural cleavage） type, with a large potential scale.
出处
《云南地质》
2008年第4期442-447,共6页
Yunnan Geology
关键词
石英脉型
金矿床
多期次多来源
构造破碎带
保山地块
云南
Au Deposit of Quartz Vein Type
Multiphase and Polygene
Structural FractureZone
Baoshan Massif
West Yunnan
