格鲁其堆山铅锌矿床是近年来新发现具有较大找矿潜力的铅锌矿床，位于得尔布干断裂中段西侧，矿化体赋存于额尔古纳河组、佳疙疸组等地层中，铅锌矿化与闪长岩、闪长玢岩具有密切的生成关系，受北东向断裂控制。热液期成矿作用大致可划分为黄铁矿±方铅矿-石英阶段（Ⅰ）,方铅矿、闪锌矿±黄铜矿-石英阶段（Ⅱ）,少硫化物-碳酸盐阶段（Ⅲ）。流体包裹体研究结果表明，石英中仅发育气液两相包裹体，成矿流体为简单中低温、低盐度的NaCl-H2O热液体系，早期成矿流体应以岩浆热液为主。主成矿阶段（Ⅱ）完全均一温度峰值集中在200 ℃~250 ℃，平均值230.2 ℃，盐度峰集中在2 %~6 %，捕获时静水压力集中在14.00~25.27 MPa，估算成矿深度为1.40~2.53 km。综合分析认为，格鲁其堆山铅锌矿床与中酸性浅成侵入体具有密切时空关系，成因类型属中温热液脉型。

Geluqiduishan Pb-Zn Deposit is a newly discovered Pb-Zn deposit with great exploration potential in recent years.It is located on the west side of the Derbugan fault section,with mineralization occurring in the strata of the Ergune River Formation,Jiageda Formation,and other formations.The lead-zinc mineralization has a close genetic relationship with diorite and diorite porphyry and is controlled by NE faults.The mineralization during the hydrothermal period can be roughly pided into pyrite±galena-quartz stage (Ⅰ),galena,sphalerite±chalcopyrite-quartz stage (Ⅱ),and low sulfide-carbonate stage (Ⅲ).Fluid inclusion studies show that only gas-liquid two-phase inclusions are developed in quartz.The ore-forming fluid is a simple,medium low temperature,low salinity NaCl-H2O hydrothermal system,with early ore-forming fluids composed mainly of magmatic hydrothermal fluids.The peak full homogenization temperatures of the main mineralization stage (Ⅱ) are concentrated in the range of 200 ℃ to 250 ℃,with an average of 230.2 ℃,and salinity peaks concentrated in the range of 2 % to 6 %.The estimated formation depth is between 1.40 km and 2.53 km,with the static hydro-pressure concentrated around 14.00-25.27 MPa.Preliminary comprehensive analysis suggests that the Geluqiduishan Pb-Zn Deposit has a close spatiotemporal relationship with medium acidic shallow intrusive bodies,and the genetic type belongs to the medium temperature hydrothermal vein type.