新疆阿尔泰山哈龙-可可托海稀有金属次级成矿带划分及进一步找矿思路  

Xinjiang, Taishan-halon KEKETUOHAI division and further prospecting of rare metal metallogenic belt of sub sea

作　　者：马德成 

机构地区：[1]新疆有色地质勘查局701队,新疆昌吉831100

出　　处：《世界有色金属》2017年第10期296-296,298,共2页World Nonferrous Metals

摘　　要：新疆阿尔泰山稀有金属伟晶岩成矿带大地构造单元属阿尔泰造山带中阿尔泰构造单元,是我国重要的稀有金属、宝石和工业白云母成矿区。成矿带各级次伟晶岩成矿单元序次完整,具有较典型的"北锂、南铍"的稀有金属矿产空间分布特征,是新疆阿尔泰山最具找矿潜力的次级稀有金属伟晶岩成矿单元。对其进行重点总结和深入研究,对找矿靶区新一轮预测工作将会产生一定的积极意义。The geotectonic unit of the rare metal pegmatite metallogenic belt in Xinjiang and Taishan belongs to the Altai tectonic unit in the Altai orogenic belt, and is an important rare metal, gemstone and industrial Muscovite ore area in china. The pegmatite metallogenic unit sequence complete metallogenic belt, rare metal mineral spatial distribution characteristics typical of the ＂North South lithium, beryllium＂, is a secondary rare metal pegmatite metallogenic unit of Xinjiang al Taishan most potential prospecting. To sum up and study it deeply, it will have positive significance for the new round of prediction of prospecting target area.

关 键 词：稀有金属 成矿带 找矿 

分 类 号：P618.3[天文地球—矿床学]