CAJ | 학술논문

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。
아북석광위우합살극사탄판괴준갈이미판괴적새미사태-동천만고생대도호대동단，구내주요출로고생계지층，구조작용강렬，암장활동빈번，침입암분포교엄，석광화여구내중산성침입암상관，광체분포주요수북동향차급단렬적공제，시암장기후기성-고중온열액형석광상。
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.