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与铜多金属矿床有关的岩体受NE(NNE)向构造为主导复合改造EW向等其他方向构造的交汇部位控制 ,矿体赋存于岩体的特定部位及其附近的破碎带中。提出矿床 (点 )分布规律为NE(NNE)向成带、近EW向成行 ,并划分出 3个次一级NE(NNE)向构造 -岩浆 -成矿带和 4个近EW向构造 -岩浆 -成矿行。
The rock mass associated with the copper polymetallic deposit is controlled by the junction of NE (NNE) tectonics, composite alteration EW and other directional structures. The ore body is located in the specific part of the rock mass and nearby crushed zone. The distribution of orebodies (points) is proposed to be NE (NNE) to zoning and nearly EW to line, and three sub-primary NE (NNE) tectono-magmatic-metallogenic belts and four near EW tectono-magmatic - Mineralization.