It is inferred that the ore-forming process of the Dengjiashan tin deposit is mainly controlled by the late-stage tectonic altered zones with the NNE trend and the major metallization pattern is the type of the tectonic altered rock zone.

• 邓家山锡矿成矿作用主要受后期北北东向构造蚀变带控制,主要矿化类型为构造蚀变岩带型。