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大兴安岭东坡中段的铜多金属矿产分布，ＮＥ成带，ＥＷ成行，ＮＷ成列，并构成多个矿化－构造带、矿化－构造块体，矿化－构造结。主要是受到区域ＮＥ向与ＥＷ向构造带构成的构造大格局和ＮＷ向与ＳＮ向构造带形成的构造小格局组合而成的“菱格网”状构造所控制。区域构造格局是铜多金属矿成矿构造的基础，据此区域性的遥感成矿预测，指出北段以找铜为主，中段以扩大银铅锌远景为主，深部找铜以及南段深部找铜的找矿方向。
The distribution of copper polymetallic minerals in the middle section of the east slope of the Greater Hinggan Mountains is characterized by NE-banding, EW-trending and NW-trending, and constitutes multiple mineralization-tectonic belts, mineralization-tectonic blocks, mineralization-structural knot. It is mainly controlled by the “rhombic” structure formed by the combination of the regional NE structural structure with the EW structural belt and the structural small structure formed by NW and SN structural belts. According to regional remote sensing metallogenic prediction, it is pointed out that the northern section is dominated by copper, while the middle section is dominated by the expansion of the silver, lead and zinc prospects, the deep looking of copper and the deep section of the southern section Looking for copper prospecting direction.