Abstract: There are two series of Cu, Au deposits,the stratiformed deposits and the intrusive-related ones in the mineralization belt of the middle and lower reaches of the Yangtze River area. Comparative studies on forming geodynamic backgrounds, geological and geochemical conditions of the ore-forming systems have been undertaken in this paper. The stratiformed deposits were formed in Hercynian period by submarine exhalation-sedimentation (SEDEX) of hot brine through the synchronous basement faults in a tensional environmental, and the intrusive-related deposits were formed in Yenshanian in a tensional or a transitional period to tensional environment during the upper mantle doming by water-rock interaction and complex transport-chemical reaction dynamic processes, the ore-forming fluids were mainly magmatic water from melt-fluid partition and some meteoric water.

Key words: fluid ore-forming system, forming conditions of ore deposit, metallogenesis, copper gold deposit, the middle and lower reaches of the Yangtze River area

摘要： 长江中下游铜、金成矿带是我国最重要的金属成矿带之一。成矿流体系统形成的地球动力学背景及地质地球化学条件对比研究表明，赋存于石炭系中的层状铜、金矿床是海西期拉张背景下热卤水沿同生断裂经喷流作用形成的海底喷流(热水)沉积矿床；与燕山期中酸性侵入岩有关的铜、金矿床是在上地幔隆起、张性或向张性过渡背景下形成的，是中酸性岩浆经熔体流体分离作用形成的岩浆热液与大气降水混合，经水-岩作用等复杂的输运和化学反应耦合过程的动力学产物。

关键词: 成矿流体系统, 成矿条件, 矿床成因, 铜, 金矿床, 长江中下游