摘要
红山南金矿位于准噶尔板块准噶尔微板块觉罗塔格晚古生代沟弧带与大南湖晚古生代岛弧带二者的中间区域上,属于康古尔塔格-镜儿泉Cu、Ni、Mo、Au成矿带,是东天山地区重要的石英脉型金矿床之一。本文通过对该矿地质特征进行分析,探讨其矿床成因,并对其找矿远景进行论述,以期为区内找矿工作提供参考。
The red Shannan gold deposit is located in the middle area of the Late Palaeozoic island arc belt of the Junggar plate Junggar micro plate jagrotagar and the late Paleozoic island arc belt of the great Nanhu lake.It belongs to the Cu,Ni,Mo and Au metallogenic belt of the gualtagg-Guer spring.It is one of the important quartz vein type gold deposits in the East Tianshan area.Based on the analysis of the geological characteristics of the mine,the genesis of the deposit is discussed,and its prospecting potential is discussed in order to provide reference for the prospecting work in the area.
作者
王毅
弓小平
李晓光
WANG Yi;GONG Xiao-ping;LI Xiao-guang(College of Geology and mining engineering,Xinjiang University,Urumchi 830049,China)
出处
《世界有色金属》
2018年第10期103-103,105,共2页
World Nonferrous Metals
基金
"新疆东准噶尔卡拉麦里金矿带成矿流体特征及其与侵入体的关系研究"(编号41462004)资助
关键词
红山南金矿
地质特征
矿床成因
找矿远景
Red Shannan gold deposit
geological characteristics
ore genesis
prospecting potential
