中国蒙古各地块大致于印支运动末期(210Ma)重新聚合,成为劳亚超大陆,即二叠纪&三叠纪泛大陆北支的一部分。
China and Mongolia were on the whole re-assembled after the Indosinian orogeny to become part of the Laurasia Supercontinent , which was the northern half of the Permian-Triassic Pangaea .