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铜厂铁矿是一个磁铁矿矿床。这个铁矿作为与热液活动有关的矿床,构造控制的重要性从未出现异议。但与铁矿形成过程自始至终密切相关的构造条件,从辩证的观点来看,也不是固定不变的,同样存在着一个发展演化的过程。构造条件在铁矿形成的不同阶段起着不同的作用。铜厂铁矿位于秦岭纬向构造带南部边缘。矿区西部该构造带南缘表现为一系列向南突出的弧形构造。矿区的骨干构——造铜厂背斜为文县弧形构造东翼的次级构造;南
Copper plant iron ore is a magnetite deposit. As an ore deposit associated with hydrothermal activity, this iron ore has never been in dispute as to the importance of tectonic controls. However, structural conditions that are closely related to the formation of iron ore from the beginning to the end are not fixed from a dialectical point of view. There is also a process of development and evolution. Tectonic conditions play different roles in different stages of iron ore formation. Copper plant iron ore located in the Qinling Mountains latitudinal tectonic belt south edge. The south margin of the tectonic belt in the west of the mining area is characterized by a series of arc-shaped structures protruding southwards. The backbone structure of the mining area - the anticline of the copper fabrication plant is the secondary structure of the eastern wing of Wenxian arch structure; south