The metallogenic type of Gangdise belt in Tibet is porphyry copper-molybdenum deposit primarily, the genesis of epithermal deposit or magmatic hydrothermal deposit has not been paid enough attentions.

• 摘要西藏冈底斯带主要成矿类型以斑岩型铜钼矿为主，对浅成低温热液或岩浆热液型矿床的成因研究相对较小。