本文从中国铜矿的地理分布出发,通过对矿点密度和断裂密度等值线的相关性分析,探讨了铜矿的空间分布及其与断裂带的关系,得出:断裂密度在(60,220)区间的铜矿点占总数的81.9%;在距断裂带20.76假定单元内(实际距离为86km)集中了大约83%的铜矿点。由此可见,断裂带与铜矿区带的展布有关,对铜矿床分布的控制作用明显。 Based on the geographical distribution of copper mines in China, the relationship between ore deposit density and fault isoline is analyzed. The spatial distribution of copper deposits and its relationship with fault zones are discussed. The results show that the fracture density is between (60, 220) The copper deposits in the interval accounted for 81.9% of the total; about 83% of the copper deposits were concentrated in the 20.76 tectonic fault zone (actual distance of 86km). Thus, the fault zone is related to the distribution of the copper ore zone and has obvious control over the distribution of the copper deposit.