摘要
万宝源斑岩钼矿位于石柱子花岗闪长岩体的东缘接触带上,受鸭绿江构造带和周家屯—万宝构造带的控制,矿床规模目前达到中型。研究认为该钼矿及其周围地带存在进一步寻找Mo、Cu、Au等矿产资源的空间。文章分析了矿床形成的区域地质背景,矿床地质特征,结合同位素特征,从成矿流体角度探求该矿床的成因机制,为下一步寻找矿靶区提供指导。
Wanbaoyuan Mo deposit is located at the contacting zone of eastern margin of granodiorite in Shizhuzi,which is controlled by Yalujiang and Zhoujiatun-Wanbao structrual belts,with the deposit reaching middle scale.The study has believed that there is a further prospecting potential for Mo,Cu,Au mineral resources in this Mo deposit and its periphery.After analyzing the regional geological background for the formation of this deposit,geological characters of this deposit,combined with isotopic features,the pap...
出处
《矿产与地质》
2009年第2期142-146,共5页
Mineral Resources and Geology
关键词
斑岩钼矿
石柱子花岗闪长岩体
成矿流体
万宝源
辽宁
porphyry Mo deposit
Shizhuzi granodiorite rockbodies
ore-forming fluid
Wanbaoyuan
Liaoning
