四千至五百万年前，印度大陆漂移与欧亚大陆发生碰撞，喜马拉雅山脉隆起。
Between 40 and 50 million years ago, India drifted right into Eurasia, raising the Himalayan Range.
位于下地幔源热区之上的中国东部大陆，发生隆起、破裂、向洋漂移。
The east China continent located over the heat source of the lower mantle was uplifted, broken and drifted toward the ocean.
皖南地区的江南隆起带，在震旦纪—中三叠世与周边一样处于被动大陆边缘海相环境。
Like surrounding areas, the Jiangnan uplift belt in southern Anhui was situated on a passive continental margin during Sinian to Middle Triassic.
应用推荐