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构造对楚雄盆地砂岩铜矿床的控制主要表现在三个层次:盆地构造演化控制了中生代到新生代沉积建造的发育,形成与矿化密切相关的三色建造,同时控制了盆地的古地理格局。基底断层和同生断层控制区内矿带的分布,矿区内的断裂构造和褶皱构造直接控制了矿体的形态和产状。
Structural control of the sandstone-type copper deposits in the Chuxiong Basin is mainly manifested in three levels: the tectonic evolution of the basin controlled the development of the Mesozoic to Cenozoic sedimentary structures, formed the three-color construction closely related to mineralization, and controlled the paleogeographic structure of the basin . The distribution of orebodies in the basement fault zone and the synsedimentary fault control zone and the fault structure and fold structure in the mine area directly control the shape and occurrence of the ore body.