摘要
杨树沟金矿为中低温热液型,呈不规则脉状产出,严格受断裂构造控制.控矿断裂主要为北东向、北西向两组,断裂性质以压性为主,可以作为本区寻找新矿体的构造标志.
The Yangshugou gold deposit of meso-epithermal type occurs as irregular quartz veins strictly controlled by faults.The controlling faults are mainly NE and NW trending compressive fractures,which can be used as the structural indicators for the exploration of orebodies in the area.
出处
《地质与资源》
CAS
2014年第A01期134-136,共3页
Geology and Resources
关键词
含金石英脉
断裂构造
金矿
找矿标志
河北省
auriferous quartz vein
fault
gold deposit
prospecting indicator
Hebei Province
