The Jiama copper polymetallic deposit, located in the middle part of the Gangdise metallogenic belt, has tungsten anomalies and local enrichment. However, very insufficient research work has been devoted to tungsten and tungsten minerals. In order to make remedy in this aspect, the authors probed into the variation of tungsten content with the depth, and made microscope identification and electron microprobe analysis. The results show that tungsten in Jiama is concentrated in the deep skarn type ore body rather than in the middle and shallow ore body. Therefore, the authors hold that there is only scheelite in Jiama, with no wolframite existent. Tungsten prospecting is promising in Gangdise, as evidenced by the continuous discovery of tungsten anomalies/ore spots in the skarn-type Cu-Mo polymetallic deposits.