摘要
阿北锡矿位于哈萨克斯坦板块准噶尔微板块的赛米斯台—东泉晚古生代岛弧带东段,区内主要出露古生界地层,构造作用强烈,岩浆活动频繁,侵入岩分布较广,锡矿化与区内中酸性侵入岩相关,矿体分布主要受北东向次级断裂的控制,是岩浆期后气成—高中温热液型锡矿床。
Aber tin ore which is located in the Kazakhstan sector of the Junggar micro Zeumes Taiwan-East Spring Late Paleozoic island arc with the eastern section of the district is mainly exposed Paleozoic strata. Magmatic activity is fre-quent,has a wide distribution intrusive rocks. The distribution of the ore body is controlled by NE second faults.
出处
《资源环境与工程》
2014年第5期660-662,共3页
Resources Environment & Engineering
关键词
阿北锡矿
断裂控制
岩浆期
热液型锡矿床
Aber tin ore
fracture control
magmatic period
hudrothermal-type tin deposit
