内蒙古自治区水泉沟果园铁铜矿成矿特征分析  

Analysis on Mineralization Characteristics of Guoyuan Iron and Copper Deposit in Shuiquangou Area in Inner Mongolia Autonomous Region

作　　者：武兴龙[1] 陈东 于延秋[1] 王广[1] 

机构地区：[1]石家庄经济学院,河北石家庄050000 [2]山东省第五地质矿产勘察院,山东泰安271000

出　　处：《山东国土资源》2014年第12期13-16,共4页Shandong Land and Resources

摘　　要：研究区位于内蒙古大兴安岭南段,属古亚洲成矿带与环太平洋成矿带复合叠加部位,通过矿产地质调查,发现该区内有Fe,Cu等多金属矿化现象,通过对研究区岩石特征、物化探异常、矿体特征等分析,确定该地区为岩浆热液型铁铜矿床,有良好的成矿前景,为该区进一步寻找隐伏矿床提供依据。The study area is located in the south of Greater Khingan Range in Inner Mongolia Autonomous Region.It belongs to superposition part of the Paleo Asian metallogenic belt and the ircum Pacific metal-logenic belt.Through geological survey of mineral resources,it is found that there are Fe,Cu and other multi metal mineralization in this area.According to analysis on rock characteristics,geophysical and ge-ochemical anomalies and ore bodies characteristics,it is regarded that iron and copper deposit in this area is magma hydrothermal type with good metallogenic prospects.It will provide the basis for the further explo-ration of concealed ore deposits in this area.

关 键 词：成矿特征 铁铜矿点 内蒙古水泉沟果园 

分 类 号：P618.41[天文地球—矿床学]