呼斯特岩体矽卡岩型铜铁矿成矿地质特征及找矿潜力分析  

ANALYSIS OF METALLOGENIC REGULARITY OF SKARN TYPE COPPER-IRON DEPOSIT AND MINERAL EXPLORATING POTENTIAL OF HUSITE ROCK IN JINHE COUNTY,XINJIANG

作　　者：万阈[1] 袁永江[2] 袁鹏[1] 宋云辉[1] 

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局第七地质大队,新疆乌苏833000 [2]新疆维吾尔自治区地质矿产勘查开发局,新疆乌鲁木齐830000

出　　处：《新疆地质》2011年第1期50-54,共5页Xinjiang Geology

基　　金：新疆维吾尔自治区地质勘查中央专项资金项目(ZXZKC2007-4;ZYZXKC2008-6);新疆维吾尔自治区地质勘查基金项目(T10-3-6)共同资助

摘　　要：论述了呼斯特岩体成矿地质背景,以艾木斯呆依铜铁矿床为例,叙述矽卡岩型铜铁矿成矿地质特征,从岩体成矿地质条件、矿化特征和含矿性出发,指出岩体主攻矿床类型为矽卡岩型,主攻矿种为铁、铜、铅锌、钼、钨,找矿有利地段为岩体南东部凹陷部位,总体找矿潜力较大.On the basis of the comprehensive information analysis of metallogenic regularity of AIMUSIDAIYI copper-iron deposit,this paper is talking about the mineralizing geology background of HUSITE rock and mineralization characreristic of skarn type copper iron deposit.It points out that the main explorating deposit type is skarn deposit,the main element is Fe,Cu,Pb,Zn,Mo,W.There is a good potential of mineral exploration at South eastern in the subside position of the HUSITE rock..

关 键 词：呼斯特 矽卡岩型铜铁矿 成矿特征 找矿潜力 

分 类 号：P618.41[天文地球—矿床学]