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从地质上看,攀西地区是个古老的大陆裂谷,攀西地区的成矿作用,主要受古裂谷构造控制。这条南北向的古裂谷,向北经龙门山、鄂尔多斯西缘,穿内蒙入蒙古人民共和国后可与贝加尔湖裂谷相连,向南经红河裂谷而连南海与中印半岛间的断裂带,构成全球性南北向锯齿状裂谷系的重要分子。裂谷有其发生发展消亡的演化过程,因而受裂谷构造控
Geologically speaking, the Panxi area is an ancient continental rift and the metallogenic process in the Panxi area is mainly controlled by the ancient rift structure. This ancient north-south paleo-rift goes northward through Longmenshan and the western edge of Ordos. It can be connected to the Baikal rift valley through Inner Mongolia to the People's Republic of Mongolia, south to the Red River rift, and even to the break between the South China Sea and the Sino-Indian Peninsula Belt, constitute a global north-south serrated rift system of important molecules. Rift Valley has its development and disappearance of the evolution process, which is controlled by the Rift Valley