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大厂是中国著名的锡-多金属矿床。该矿所在的丹池矿带正处在一级构造东南地洼区西段黔桂地洼列的桂西地洼。它经历了地槽(前泥盆纪)、地台(泥盆纪至三叠纪)和地洼(三叠纪末至现代)不同的大地构造发展阶段,形成相应的构造层和复杂的构造-岩浆和成矿带。
Dachang is a famous tin-polymetallic deposit in China. The mine is located in the Danchi belt is located in the construction of the western part of the depression in the southeast of Guizhou and Guangxi to depression depression of Guangxi West depression. It experienced different tectonic development stages of the Trough (Pre Devonian), Platform (Devonian to Triassic) and Diwa (Late Triassic) to form the corresponding structural layers and complex structures - Magma and metallogenic belt.