1：5万水系沉积物测量表明，该区属浅成低温热液型金多金属成矿区，除受构造控制外，岩浆岩、地层亦有控矿作用。金矿主要分布在裂谷带中，成矿潜力巨大，测区西部杨梅山中部支壁找铜金、东南部大得克找铅锌有较好前景。%According to the 1 ： 50000 sediment survey of water system, this area belongs to the Au muhime- tallic epi -metallogenesis province of low T hydrothermal type. The metallogenesis is controlled by magmatic rock and strata besides structure. The Au deposit is mainly in the rift zone, with great metallogenetic potentiality. There are good prospecting potentiality separately for Cu, Au at Yangmeishan in the west and at Zhibi in the cen- tral part; for Pb -Zn at Dadekei in SE.
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