摘要
甘肃省天水市李子园金矿床处于西秦岭北段多金属成矿带,近年来通过钻探、坑探工程对其深部及外围矿体的控制,对该地区矿床成因有新的认识。本文通过对区内成矿模式的研究,并结合野外地质现象进行分析和讨论,以期对下一步勘查找矿工作给予指导意见。
The Li Zi Yuan gold deposit in Tianshui,Gansu province is located in the polymetallic metallogenic belt in the northern section of West Qinling Mountains.In recent years,a new understanding of the genesis of the deposit in this area has been made by the control of the deep and peripheral orebodies through drilling and pit exploration engineering.In this paper,the study on the metallogenic model in the area and the field geological phenomena are analyzed and discussed in order to give guidance to the next exploration and prospecting work.
作者
张永哲
屈海浪
成山林
ZHANG Yong-zhe;QU Hai-lang;CHENG Shan-lin(Beijing Jin you Geological Survey Co.,Ltd.,Beijing 100011,China)
出处
《世界有色金属》
2018年第11期121-122,共2页
World Nonferrous Metals
关键词
金矿
韧性剪切带型
斑岩型
李子园
西秦岭
gold deposit
ductile shear zone type
porphyry type
Li Ziyuan
western Qinling Mountains