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河南省卢氏县葫芦山铅锌矿区位于华北地区地台南缘,在该地区,以黑沟-栾川断裂为界,与南为秦岭地槽区的北秦岭分区,与北是华北地平台区的豫西分区。该区岩浆活动不断,断裂构造发育。石各种矿物质金属矿床的成矿带。该区所处地带经历了长期多次的构造运动以及火山爆发和大规模岩浆侵入作用,且为秦岭地槽与华北地台衔接地带,大量裂隙为含矿热液熔岩的运移和聚集提供了通道与空间,是成矿的主要条件。一、控矿因素
The Lushan County Hulushan lead-zinc mine in Henan Province is located in the southern margin of the platform in North China. In this area, it is bounded by the Heigou-Luanchuan fault and is divided into North Qinling in the south by the Qinling terrain and North with the North China Platform West of the partition. The magmatic activity in the area is continuous and the fault structure develops. Stone mineralized metal mineralization belt. The zone in this area experienced many tectonic movements and volcanic eruptions and large-scale magmatic intrusions for a long period of time. It provided a link between the Qinling Gully and the North China Platform and a large number of fractures for the migration and accumulation of ore-bearing hydrothermal lava Channel and space, is the main conditions for mineralization. First, control factors