CAJ | 학술논문

　　西藏墨竹工卡县哈海岗钨钼多金属矿床是近年来在冈底斯成矿带首次发现的矽卡岩型钨钼矿床。笔者主要介绍了该矿区的地质特征、地球物理特征、地球化学特征，通过对该矿床进行成矿地质条件、地球物理特征、地球化学特征综合分析，确定矿床类型和范围。经工作评价，查明该矿床钨钼资源量已达大型矿床规模。该矿区的找矿经验对在冈底斯成矿带上寻找该类型钨钼矿具有指导意义。
　　서장묵죽공잡현합해강오목다금속광상시근년래재강저사성광대수차발현적석잡암형오목광상。필자주요개소료해광구적지질특정、지구물리특정、지구화학특정，통과대해광상진행성광지질조건、지구물리특정、지구화학특정종합분석，학정광상류형화범위。경공작평개，사명해광상오목자원량이체대형광상규모。해광구적조광경험대재강저사성광대상심조해류형오목광구유지도의의。
The Hahaigang W-Mo polymetallic deposit in Mozhugongka county of Tibet is the first skarn type W-Mo de-posit that is discovered in Gangdes metallogenic belt in recent years. An account of the geological, geophysical and geochemical characteristics of this mining area is given. The deposit’s type and scale are ascertained after a compre-hensive analysis on its geological, geophysical and geochemical characteristics. The deposit is graded as a large de-posit according to the amount of tungsten and molybdenum resources. The experience that acquired during prospec-ting in this mining area provides guidance for seeking the same type of W-Mo deposits in Gangdese metallogenic belt.