摘要
通过找矿工作的实践 ,证实塔儿山—二峰山地区金矿体产于破碎带内 ,并认为破碎带构造复杂 ,硅化、黄铁矿、褐铁矿化 。
WT5BZ]It is proved by prospecting work that the Gold orebodies occur in fracture zone.It is considered that the structure of fracture zone is complicated and silicification, pyrite limonite, and deep altered districts are important indications for Gold deposit prospecting. [WT5HZ]
出处
《矿产与地质》
2000年第6期365-379,共15页
Mineral Resources and Geology
关键词
破碎带
主断面
金矿床
矿床地质
载金脉体
找矿标志
WT5BZ]Taershan Erfengshan
Fracture zone
Main profole
Gold deposit
Geological Character
