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中条山是我国重要的铜矿产区之一.篦子沟类型铜矿床,在中条山铜矿中占有重要地位.该区这一类型矿床产地多,分布广,含铜品位高.因此对该类型铜矿进行深入细致地研究具有重要的意义.一、区域地质简介中条山为前震旦纪变质褶皱区.洓水杂岩构成古老的结晶基底,该基底具有明显的地台型特征;其上的绛县群、中条群、马村群、担山石群属地槽型沉积,震旦系具有地槽-地台过渡型沉积特征.
Zhongtiaoshan is one of the most important copper mineralization areas in our country.The Goupizigou type copper deposit occupies an important position in the Zhongtiaoshan copper deposit, which has a large area and wide distribution and high copper bearing grade. It is of great significance to study this type of copper deposit in depth.First, the introduction of regional geology Zhongtiaoshan is a pre-Sinian metamorphic fold zone, in which the Huangshui complex forms an ancient crystalline basement with obvious terraces ; The Jiangxian Group, Zhongtiao Group, Macun Group, and Danshanishi Group have the trough-type sediments, and Sinian has the sedimentary characteristics of the trough-platform transitional type.