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钼矿是悬岭后多金属矿区近几年新发现的矿产,主要产于早元古代连山关～高家沟花岗杂岩体内的解理裂隙中,钼矿石呈浸染状或细脉状产出,矿床类型为斑岩型,成因与中生代燕山期白水寺花岗岩体密切相关。对其成矿特征及成因的研究对区域寻找钼矿产具有重要的指导意义。
Molybdenum ore is a new mineral discovered in the polymetallic mines after the hanging ridge in recent years. The molybdenum ore is mainly found in cleavage cracks in the Early Proterozoic Lianshanguan ~ Gaojiagou granite complex. The molybdenum ore is disseminated or small veins The ore-forming type is porphyry type, which is closely related to the Mesozoic Yanshanian Baishui Temple granite. The study of its metallogenic characteristics and genesis has important guiding significance for the area looking for molybdenum mineral.