喀拉通克铜镍矿地球物理特征及成矿预测研究  

Study of Metallogenic Forecast and Geophysical Characteristics in Copper-nickel Mine of Kalatongke

作　　者：佟铁钢[1] 胡祥昭[1] 柳建新[1] 

机构地区：[1]中南大学地质系,湖南长沙410083

出　　处：《西部探矿工程》2004年第9期105-106,共2页West-China Exploration Engineering

摘　　要：新疆喀拉通克镍多金属成矿带位于中亚壳体北东部的阿尔泰地洼区与准噶尔地洼区的过渡部位。断裂发育 ,地质构造复杂 ,岩浆活动频繁、岩性复杂 ,成矿地质条件优越。研究和掌握控岩、控矿构造规律 ,提出矿区的找矿模式 ,寻找出适合矿山发展的大型—超大型深部隐伏铜镍矿已经成为维持矿山可持续发展的当务之急。The nickel and other kind of metals mine of Kalatongke District locates in the transition area between Mid-Asia Plate east-north of A'E'Tai Geodepression Zone and Zun'Ge'Er Geodepression in Xinjiang. It is fragmentation development,geologic structure complexity,magmatism frequency and minerogenetic geological conditions superiority. It has become urgent matter maintaining the mine's sustained development to study and master the structural regularity of controlling rock and controlling orebody,bring forward the mode of exploring mine in mining area,find a large or super-large scale of deep concealed copper-nickel mine.

关 键 词：铜镍矿 成矿预测 新疆 

分 类 号：P612[天文地球—矿床学]