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根据新藏公路沿线实际观察资料及前人研究成果，着重通过库地北构造带两侧变质岩、岩浆岩及构造古环境特征的对比，以及对构造带中蛇绿岩的地质特征和形成环境的分析，初步探讨了该构造带的大地构遣演化。认为库地北构造带为古昆仑洋盆消减、封闭的最终位置，是形成于志留纪的板块聚合碰撞缝合带，代表着早古生代阶段塔里木板块的南部边界，也是控制塔里木盆地西南部和西昆仑山地区区域构造格架的重要构造带。
Based on the observation data along the Xinshin Highway and the research results of the predecessors, the author compares the characteristics of metamorphic rocks, magmatic rocks and tectonic paleoenvironments on both sides of the Kudi North structural belt, and analyzes the geological characteristics and formation environment of the ophiolite in the structural belt Analysis of the tectonic zone of the evolution of the earth’s tectonics. It is considered that the Kuduigabe structural belt is a subducted and closed final position of the ancient Kunlun ocean basin. It is a polymerized collision suture zone formed in the Silurian plate, representing the southern boundary of the Tarim plate in the Early Paleozoic stage and also the southwestern and western part of the Tarim Basin The Important Tectonic Belt of the Tectonic Framework in the Kunlun Mountains Region.