青分岭金矿床位于北祁连NW向金多金属成矿带中段。根据青分岭金矿床的地质特征,分析了控矿条件,认为金矿受下奥陶统(O1)火山岩系地层、NWW向断裂、碱性二长岩控制,其成因为多期成矿的中一中低温热液型金矿床,进而提出找矿方向,指出青分岭金矿深部及外围细浪沟、人熊沟一带需要进一步开展勘查找矿工作。
Qingfenling gold deposit is located in the middle of the north Qilian gold-polymehallic metallogenic belt. By analyzing the geological characteristics, we discussed ore-controlling conditions and prospecting direction of the deposit. Qingfenling gold deposit is a multi-period meso-epithermal deposit controlled by lower ordovician system volcanic series, NNW trending faults and alkalic monzonite rock. The depth of Xilanggou and Renxionggou nearby the deposit have good prospecting potential.