摘要
英山地区金矿发育在沂水-汤头断裂的次级断裂破碎带上,主要有破碎带蚀变岩型与含金石英脉型两种,矿体规模小,矿石品位变化大。
The gold deposit of Yingshan area developed in the secondary fracture zone of Yishui-Tangtou fracture including fracture zone altered rock type and auriferous quartz vein type. The size of the ore body is small and grade of ore is variable.
作者
郭长胜
GUO Chang-sheng(The 7th institute of geology & mineral exploration of Shandong Province,Linyi,276006,Chin)
出处
《世界有色金属》
2017年第6期211-212,共2页
World Nonferrous Metals
关键词
英山金矿
沂水-汤头断裂
破碎带蚀变岩
含金石英脉
Yingshan
Yishui-Tangtou fracture zone
fracture zone altered rocks
auriferous quartz vein