CAJ | 학술논문

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。
연구구위우내몽고대흥안령남단，속고아주성광대여배태평양성광대복합첩가부위，통과광산지질조사，발현해구내유 Fe，Cu 등다금속광화현상，통과대연구구암석특정、물화탐이상、광체특정등분석，학정해지구위암장열액형철동광상，유량호적성광전경，위해구진일보심조은복광상제공의거。
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.