关键词: 中国大陆, 盆地类型, 太平洋板块, 机制探讨, 边缘海盆地, 构造带, 特提斯, 活动大陆边缘, 转换断层, 拉裂盆地

Abstract: Southeastern China continental margin has undergone a complicated convergence process of the Eurasian plate with the Pacific plate and Tethys plate.With the subduetion of the Pacific plate under the Eurasian plate,the Eastern China continental margin crust was subject to aregional tension stresses that caused the breakdowrn,spreading and subsidence of the back-arc basement and formed a series of intra-arc basins,margin sea basins.and rift basins.The East China Sea basin grew up under the influence of compressional stresses caused by the collision between Luzon and Taiwan in the later stage and a fore-continental basin was formed.