摘要
Dachang tin-polymetallic deposit is located in the middle of Nandan-Hechi metallogenic belt, which is one of the famous tin mine in the world. There are three mineralized zone in the ore field from west to east, which is tin-polymetallic belt in the west and east, the Skarn type zinc-copper ore deposit in the middle. They are obviously asymmetric on horizontal direction, and also have greatly different on mineral assemblages and orebody shape. By analyzing the structural configuration and comparing physicochemical property of ore-forming fluid in each metallogenic zoning, it illustrates metallogenic zoning characteristics in Dachang ore field and interprets the orebody shape differences in vertical on different ore belt.