新疆野马泉阿北锡矿的矿化规律及找矿标志  

Mineralization Law and Prospecting Criteria of Aber Tin Ore in Yemaquan,Xinjiang Province

作　　者：郭燕 曹东梅 王斯林 

机构地区：[1]新疆地矿局物化探大队,新疆昌吉831100

出　　处：《资源环境与工程》2014年第5期660-662,共3页Resources Environment & Engineering

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.

关 键 词：阿北锡矿 断裂控制 岩浆期 热液型锡矿床 

分 类 号：P618.44[天文地球—矿床学]