西天山赛里木湖地区东卡尔阿依铅锌矿的发现及找矿意义  

On the Discovery and Prospecting Significance of the Dongkaerayi Pb-Zn Deposit in the Sailimu Lake area of the West Tianshan

作　　者：王海涛[1] 吴福泉 夏明[1] 李鑫[1] Wang Haitao;Wu Fuquan;Xia Ming;Li Xin(No.1 Geological Surveying institute of Xinjiang Surveys of Geology,Urumqi,Xinjiang,830011,China)

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局第一区域地质调查大队,新疆乌鲁木齐830013

出　　处：《新疆地质》2021年第2期236-239,共4页Xinjiang Geology

摘　　要：东卡尔阿依铅锌矿位于西天山赛里木湖以南,属赛里木湖铜铅锌金成矿带,赋存于中元古界青白口系碳酸盐岩地层中,岩控和层控特征明显,与岩浆活动无明显联系。成矿带矿石品位高,矿石矿物以菱锌矿为主,具富锌少铅特点。青白口系属台地相沉积环境,为镁、硅质碳酸盐岩夹碎屑岩建造。通过总结该矿点矿化特征,结合赛里木湖周边1∶5万化探异常特征,认为中元古界青白口系是该区寻找铅锌矿最有利层位。The Pb-Zn ore of Dongkaerayi is located in the south of Sailimu Lake in the West Tianshan,It belongs to Sail-imu Lake Cu-Pb-Zn-Au copper and metallogenic belt.It mainly associated with Neoproterozoic Qingbaikou Period car-bonate formation,the rock-and strata-controlling characteristics were significant,and it is not obvious and direct contact to the magmatism.The ore grade is high,its mineral constituents is smithsonite,which is rich in zinc and less lead.Its depo-sitional environment was platform facies in the Qingbaikou Period,which is magnesium-quartz carbonate rock construc-tion with fragments rock construction.We figured the cretaceous of Qingbaikou Period are the favourable formations for searching Pb-Zn deposits in the region,by concluded the mineralization features of the Dongkaerayi ore,and analysed the regional geochemical anomalies of the Sailimu Lake area.

关 键 词：东卡尔阿依 层控型铅锌矿 找矿方向 

分 类 号：P618.42[天文地球—矿床学] P618.43[天文地球—地质学]