中文摘要：

华南陆块由扬子地块和华夏地块组成,是全球罕见的世界级多金属成矿省,成矿潜力巨大。华南陆块的形成和演化,受到了很有特色的陆内大陆动力学过程的影响,其中的晚古生代地幔柱成矿系统、中生代大面积低温成矿系统、中生代大花岗岩省成矿系统等陆内成矿系统,在全球背景中很有特色,是全球研究陆内成矿作用的理想基地。对华南陆块地质历史时期的大陆动力学过程如何制约上述成矿作用的发生,以往已开展不同程度的研究并取得重要成果。笔者在论述这些研究进展的基础上,提出了三大成矿系统需要进一步研究的一些科学问题。

英文摘要：

The South China continent including the Yangtze Block and the Cathaysia Block is an uncommon world-class polymetallic metallogenic province with great ore-forming potential.The formation and evolution of the South China continent had undergone specific intra-continental dynamic processes,in which the Late Permian plume-related metallogenic system,the Mesozoic huge low-temperature metallogenic system and the metallogenic system of the Mesozoic great granite province are quite distinctive in the world.Thus,the South China continent becomes an ideal international base for studying the intra-continental mineralization.The studies, in various levels,of how the continental dynamic processes over different geological time control the mineralization in the South China continent have been carried out and have had important achievements.On the basis of these studies,this paper presents the major scientific questions for further research on the three metallogenic systems.