Outline of Regional Metallogeny of Ore Deposits Associated with the Mesozoic Magmatism in South China

South China underwent six stages of tectonic evolution and formed favorable metallogenic geological environments, the Mesozoic in particular, within which six tectonic magmatic belts can be concluded: the Middle and Lower Reaches of the Yangtze River, the Jiangnan Uplift, the Northeast Jiangxi(the eastern Qin-Hang belt), the Wuyi-Yunkai, the Nanling and Coastal Areas of Southeast China. According to geological tectonic units and environments, metallogenic specialization of the magmatism, closely genetically related deposits, the deposits formed in the Mesozoic in South China have been divided into five metallogenic series. The characteristics of each metallogenic series have been summarized, and the boundary and transition or overlapping features of these metallogenic series have also been analyzed. On this basis, the spatial-temporal distribution and evolution, the relationship between each metallogenic series and crust-mantle interaction, the relationship between the mineralization in Mesozoic and the collision between the North China and the Yangtze Plates in Indosinian, the remote effects of the Paleo-Pacific Plate subduction underneath the Eurasian Plate in Yanshanian, and important contributions of the mantle tectonic movement in Yanshanian to magmatic mineralization in South China, etc., have been discussed in this paper.