论文部分内容阅读
矿区位于西坪向斜之北翼,区内出露地层主要为古元古界银鱼沟群一套中浅变质岩系,次为新太古界登封岩群和中元古界汝阳群和古生界寒武系部分地层,区内褶皱复杂,断裂构造相对简单,岩浆活动频繁,铜、铁矿点较多,成矿条件极为有利。矿区内共发现4条铜矿化带,矿化带受控因素主要
The mining area is located in the north wing of the Xiping syncline. The exposed strata in this area are mainly a series of medium-metamorphic rocks of the Yinyuangou Group in the Paleoproterozoic, followed by the Dengfeng Group in the Neoplyozoic and the Ruyang Group in the Middle Proterozoic Some parts of the Paleozoic Cambrian strata, the fold complex, the fault structure is relatively simple, frequent magmatic activities, copper, iron ore more points, extremely favorable metallogenic conditions. A total of four copper mineralization zones were found in the mining area, with the main controllable factors of the mineralization zone