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甘珠尔庙银多金属矿区地处内蒙大兴安岭东坡南段,位于黄岗梁—甘珠尔庙铜多金属成矿带北东部、白音诺—甘珠尔庙银铜多金属成矿亚带的北东段。矿体具有品位高而不均,厚度相对较薄而密集分布的特点,构造及其节理裂隙控矿作用明显,矿体视电阻率和视充电率异常表现为低阻高极化组合特征,推测密集蚀变脉群的深部可能存在与本区成矿有关的隐伏岩体,在进一步找矿工作中应加以重视。同时,在各矿化脉体的深部交汇部位是找矿的最有利部位,在今后找矿中应加强该部位的钻探验证工作。
Located in the southern section of the east slope of Daxinganling, Inner Mongolia, Ganjurumiao silver polymetallic deposit is located in the north east of the Huanggangliang-Ganjuelian copper-polymetallic metallogenic belt. The Baiyinuo-Ganjuermiao silver-copper polymetallic metallogenic belt North East section. The ore bodies are characterized by high and uneven ore grades, relatively thin and densely-distributed ore bodies, obvious ore-control effects of structures and their joints and fissures, abnormalities of apparent resistivity and apparent charging rate of ore bodies characterized by low resistivity and high polarization, and speculated There may be some hidden rock mass related to the ore-forming in the deep of the intensive alteration pulse group, which should be paid more attention in the further prospecting work. In the meantime, the most favorable site for prospecting is found at the intersections of the mineralized veins, and the drilling verification of this site should be strengthened in the future prospecting.