阿灭里根萨依铁矿地质特征  

The Discovery and its Geological Features of Amieligensayi Iron Ore Deposit in Nileke,Xinjiang

作　　者：李新光[1] 薛春纪[1,2] 王晓薇[1] 

机构地区：[1]新疆地质矿产勘查开发局第九地质大队,新疆乌鲁木齐830009 [2]中国地质大学,北京100083

出　　处：《新疆地质》2012年第3期300-303,共4页Xinjiang Geology

基　　金："十一五"国家科技支撑计划(2011BAB06B02)项目资助

摘　　要：新疆尼勒克县阿灭里根萨依铁矿位于博罗科努金、铜、铅、锌多金属(Ⅳ级)成矿带中部,形成于古生代复合岛弧环境,是近年来西天山地区发现的富铁矿之一。本文以野外生产获得的地质资料为基础,通过研究该矿区成矿地质背景、磁异常特征、蚀变带及矿体特征,分析成矿环境和成矿作用,初步认为该矿床属矽卡岩型成因类型,具良好找矿前景。The Amieligensayi iron ore deposit,is located in the Boluokenu gold-copper-lead-zinc polymetallic metallogenic belt （IV grade） which is a Paleozoic compound island-arc environment,is a newly found rich iron ore deposit in the Boluohuoluo belt,West Tianshan region.Based on the field geological data,the paper makes researches on the metallogenic geological background,magnetic anomaly characteristics, alteration zones and ore-body characteristics in the iron ore deposit, and the analysis of the metallogenic environment and ore characteristics.The Amieligensayi iron ore deposit is of the skarn-type of iron deposit in genesis and has good prospecting potential.

关 键 词：西天山 阿灭里根萨依 富铁矿 矽卡岩型 

分 类 号：P618.31[天文地球—矿床学]