摘要
库科西鲁克位于新疆西昆仑多金属成矿带,该区地质构造复杂且具有多期岩浆活动,基础地质和矿产地质研究比较薄弱。本文借助1:5万区调项目中的最新研究成果研究认为,长城系和奥陶—志留系地层和岩浆岩可能提供成矿物质来源,构造发育,岩性岩相变化带、矿化蚀变和长城系和奥陶—志留系地层是该区的找矿标志。
Kukexiluke zone belongs to polymetallic deposits belt in the west Kunlun of Xinjiang with complex geological structure and multiperiodic magmatic activities. There is weak point in research of basic geology and mineral deposits. In the paper, it is suggested that the stratum（Ch and O-S） can supply the source of metallogenic substance by the new achievement of 1：50 thousand geological and minerals survey. The inductor of this zone are structure, the variation range of lithologic charactors and lithofacies, mineralize alteration and the stratum（Ch and O-S）.
出处
《中国矿山工程》
2008年第2期49-52,共4页
China Mine Engineering
基金
新疆阿克陶县恰尔隆一带1:50000区域地质矿产调查(XJQDZ 2006-18)资助
关键词
新疆西昆仑
多金属矿床
成矿地质条件
分析
the west Kunlun of Xinjiang
polymetallic deposit
metaIIogenic conditions
analysis
