Southwest Fujian is a typical transitional area from Tethyan tectonic regime to Pacific epicontinental tectonic regime. The complex tectonic framework and varied rock-forming and ore_forming environments resulted from multiple-episode tectonic evolutionary processes. The good conditions for hydrothermal activity and deep thermal sources are attributed to multiple-episode and multiple-stage volcanic/intrusive activities for mineralization in the ore-concentrated area. The authors have summed up the time-space evolutionary regularity of mineral deposits in the area, and indicated the relationship between metallogenic series of mineral deposits and tectontc enviroment. The multiple-age, multiple_stratum, multiple_ore element and multiple-genesis mineral deposits result from varied tectonic environments.