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宁蒗白牛厂矿区位于区域性牛窝子－罗卜地帚状构造的内旋断裂带——白牛厂弧形断裂的拐折部位。由白牛厂弧形断裂伴生的低级次白牛厂帚状断裂构造带，为本区矿液运移和矿体赋存提供了良好通道和有利空间。在白牛厂喜马拉雅期含矿隐伏斑岩体与其围岩（Ｐ１灰岩）的外接触带的构造叠合地段，有望形成斑岩体外接触带热液型铅锌（银）多金属矿床。矿区铅锌矿化主要受控于白牛厂背斜轴部及其以西的白牛厂帚状构造的各弧形断裂带（以ｆ３、ｆ４、ｆ５为主），尤其是其弧形拐折至收敛地段。
Ninglang Baiguochang mining area is located in the region of the bovine rover to broom-like structure of the inner rotation fault - the white cattle arc fracture inflection point. The broom-like fault zone of the lower-level white cow associated with the arcuate rupture of the White Cattle Plant provides a good channel and favorable space for the migration of ore fluids and the occurrence of ore bodies in this area. It is expected that the hydrothermal Pb-Zn (Ag) polymetallic deposits of the in-vitro contact zone of porphyry will be formed in the structural superimposed area of the outer contact zone of the Himalayan ore-bearing porphyry and its surrounding rock (P1 limestone) in the White Cattle. The lead-zinc mineralization in the mining area is mainly controlled by the arcuate fracture zones (mainly f3, f4 and f5) of the bovine billet of the Beef Cattle Aisle Axis and its western part, especially its arc-shaped inflection To the convergence of lots.