安徽铜陵地区地处长江中下游铜、金、多金属成矿带,是国内大型铜、金矿集区之一(常印佛等,1991)。本区矿床类型多样,是成矿理论研究绝佳之地。前人在成矿流体研究中取得了丰硕的成果(肖建新等,2002;李进文等,2006),但这些成果多集中于单个矿床或矿田,尚缺乏系统地总结。铜陵地区属扬子板块北缘下扬子拗陷之相对隆起区。在稳定的前寒武纪基底之上的寒武纪至中三叠世地层形成了巨厚的沉积盖层,并成为铜、金、铁、硫等矿化的有利围岩。印支—燕山运动使本区 Tongling, Anhui Province is located in the middle and lower reaches of the Yangtze River copper, gold and polymetallic metallogenic belt, is one of the large copper and gold deposits (often India Buddha, 1991). Various types of deposits in the area, is an excellent study of metallogenic theory. The predecessors have made fruitful achievements in the study of ore-forming fluid (Xiao Jianxin et al., 2002; Li Jinwen et al., 2006). However, these achievements are mostly concentrated in a single ore deposit or ore field. However, there is a lack of systematic summary. The Tongling area is a relative uplift area of ​​the lower Yangtze depression in the northern margin of the Yangtze Plate. The Cambrian to Middle Triassic strata over the stable Precambrian basement formed a thick sedimentary cover and became favorable mineralized rocks such as copper, gold, iron and sulfur. Indochina - Yanshan movement to the area