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在板块构造理论基础上，通过区内蛇绿岩、与俯冲有关的岩浆岩及相关沉积等综合研究，对西昆仑早古生代构造演化进行了重建：震旦纪－寒武纪西昆仑从塔里木大陆分裂出去，并在它们之间形成“昆仑洋”；寒武纪－奥陶纪“昆仑洋”洋壳向南俯冲于西仑之下，形成库地俯冲带、库地弧前盆地、西昆仑早古生代火山弧及麻扎－黑卡弧后盆地；志留纪－早泥盆世，“昆仑洋”消失，西昆仑早古生代火山弧与塔里木大陆碰撞，并形成塔里木前陆冲断带和泥盆纪前陆盆地磨拉石及塔里木大陆内泥盆纪的“红层相”
On the basis of plate tectonics theory, the tectonic evolution of the Early Paleozoic in the West Kunlun was reconstructed through comprehensive study of ophiolite in the region, subduction-related magmatic rocks and related sediments: the Sinian to the Cambrian West Kunlun split off from the Tarim , And formed “Kunlun Ocean” between them. The Cambrian-Ordovician “Kunlun Ocean” oceanic crust diveped southward under the Xilun, forming the Kudu subduction zone, the Kudi pre-arc basin, the Early Paleozoic of the West Kunlun Volcanic arc and Mazar-Kurka backarc basin. During the Silurian-Early Devonian, the “Kunlun Ocean” disappeared. The Early Paleozoic volcanic arc of West Kunlun collided with the Tarim continent and formed the Tarim foreland thrust belt and Devonian The foreland basin molasse and Tarim continental Devonian “red phase”