CAJ | 학술논문

　　朗达铜矿处于雅鲁藏布江弧―陆碰撞结合带的北侧、冈底斯陆缘火山―岩浆弧南缘，属于贡嘎―加查EW向铜多金属成矿带；产于喜山期中酸性岩浆岩的断裂带中。目前发现的2条矿(化)带呈脉状、透镜状、似层状产出，且受矿区近EW向或NWW向的断裂控制。矿石构造主要以条带状、脉状及角砾状为主，部分聚合体为斑杂状或浸染状。通过对矿区地质、矿体及矿石特征仔细分析后，认为该矿床主要受构造、岩浆热液控制，且具备良好的找矿前景。
　　랑체동광처우아로장포강호―륙팽당결합대적북측、강저사륙연화산―암장호남연，속우공알―가사EW향동다금속성광대；산우희산기중산성암장암적단렬대중。목전발현적2조광(화)대정맥상、투경상、사층상산출，차수광구근EW향혹NWW향적단렬공제。광석구조주요이조대상、맥상급각력상위주，부분취합체위반잡상혹침염상。통과대광구지질、광체급광석특정자세분석후，인위해광상주요수구조、암장열액공제，차구비량호적조광전경。
Langda Cu deposit, which is part of Gonggar-Gaca east-west Cu polymetallic metallogenic belt and origi-nates in fractured zone of middle acidic magmatic rock in Himalaya Period, is located at the north of arc-land collision suture zone of Yarlung Zangbo River and on the southern margin of Gangdise epicontinental magmatic-volcanic arc. Two mineralization belts in vein, lenticular and layered shapes that discovered so far are controlled by near EW or NWW fractures in this mining area. Most ore structures are in banded, veined and brecciated shapes, while part of the polymers are in ataxitic or disseminated shapes. According to the careful analysis on geologic conditions, ore bodies and ore features of the mining area, structure and magmatic hydrothermal fluid are the major controlling fac-tors. In conclusion, this area has favorable prospecting potential.