狮子山铅锌矿床位于湖南省西部花垣铅锌矿区,大地构造上位于扬子克拉通东南缘。近年来,前人对该矿床进行了矿床成因(彭国忠,1986;李宗发,1991;刘文均和郑荣才,2000)、成矿时代(段其发等,2014)、成矿物质来源(李宗发,1992;蔡应雄等,2014)等方面的研究,获得了丰硕成果。然而,对于流体运移的驱动力以及流动方式并没有得到重视。本文根据区域构造背景,结合成矿时代, The Lion Rock Pb-Zn deposit is located in the Huayuan Pb-Zn mining area in the west of Hunan Province and is located on the southeastern margin of the Yangtze craton. In recent years, the predecessors conducted the genesis of the deposit (Peng Guozhong, 1986; Li Zongfa, 1991; Liu Wenjun and Zheng Rongcai, 2000), the metallogenic epoch (Duanfa et al., 2014), the sources of metallogenic material (Li Zongfa, 2014) and other aspects of research, has achieved fruitful results. However, no attention has been paid to the driving forces and the flow patterns of fluid migration. Based on the regional tectonic setting, combining with the mineralization era,