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东昆仑造山带从北向南依次可划分出东昆北带、东昆中混杂岩带、东昆南带、阿尼玛卿混杂岩带和巴颜喀拉带５个大地构造地层带．根据对各地层带物质建造序列和构造古地理的研究基础之上所进行的古地磁分析认为，东昆北、东昆南、阿尼玛卿３个构造单元，在海西—印支期均处于北纬１４°～２０°之间．迄今为止，三者由南而北已漂移了约１５００～２０００ｋｍ．３个构造单元在不同时期的古纬度及古纬度差反映了多岛洋盆扩张和闭合的多旋回性．从东昆中到巴颜喀拉带，其洋盆的开裂、收缩、关闭和前陆盆地的演化更替，无论在时间上和地理位置上均呈现规律性的从北向南依次迁移的特点，即在时间和平面上构成定向性构造迁移和多旋回．
The East Kunlun orogenic belt in turn can be divided into five major tectonic stratigraphic zones, namely, the East Kunqu North Belt, the East Kunqu, the East Kunqun Belt, the Animaqing Concomitant Belt and the Bayankela Belt from north to south. According to the paleomagnetic analysis based on the study of stratigraphic sequence and tectonic palaeogeomorphology in the strata, the three tectonic units of the East Kunlun Mountains, East Kunlun Mountains and Animaqing, Latitude 14 ° ~ 20 ° between. To date, the three have drifted about 1500-2000 km from south to north. The paleoclimatic and paleoclassical latitudes of the three tectonic units at different periods reflect the multi-cycle of multi-oceanic basin expansion and closure. From East Kunlun to Bayankhala belt, the cracking, shrinkage, closing and foreland basin evolution of the oceanic basins are characterized by time-varying and geo-positional regular migration from north to south, ie, Constructs directional tectonic migration and multi-cycles in time and in plane.