石槽铜矿属于具复杂矽卡岩晚期成矿特征的矿床类型。作者指出:不同规模、不同序次的构造透镜体控制着接触带附近的变矽卡岩铁铜矿体的分布和富集;构造动力在高中温热液阶段起着重要的成岩成矿作用;接触交代作用之后的变质作用具有动力和其它因素共同起作用的特征。本文认为这种动力作用下的变质矽卡岩化及其成矿不仅是矿区的重要成矿作用,而且也是主要的成矿阶段。 Shiguang copper deposit belongs to the type of deposit characterized by late stage metallogenic complex skarn. The authors point out that tectonic lenses with different scales and different orders control the distribution and enrichment of the altered skarn iron-copper ore bodies near the contact zone. The tectonic motions play an important diagenetic and mineralizing role in the high-temperature warm-liquid phase. Metamorphism after exposure to metathesis has the motivation and other factors that work together. This paper argues that the metamorphic skarnization and its metallogenesis under this dynamic action are not only important metallogenic processes but also the major metallogenic stages.