The central East Kunlun tectonic Melange belt is a polycyclic composite collisional suture zone which was formed through the neoproterozoic,terminal Caledonian and late hercynian collisional events.

• 东昆仑中部构造混杂岩带是经历了新元古代、加里东末期和晚海西期3次碰撞事件而形成的多旋回复合的碰撞缝合带。