尕怒大门帚状构造,展布于东昆仑山西段北坡那陵格勒河西岸,面积约250平方公里。它是西域系断裂带中一系列低序次旋扭构造之一,发育在元古界金水口群(Ptjn)、上奥陶统铁石达斯群(O_3ts)、上泥盆统契盖苏群(D_3qg~b)及华力西期侵入岩中,由4条规模较大的弧形断裂围绕克停哈尔北山核心地块向南东方向撒开,构成一较为完整的帚状图象(见附图)。 Gathera gate broom structure, distributed in the eastern Kunlun Mountains Shanxi Nalu Ling River on the northern bank, an area of ​​about 250 square kilometers. It is one of a series of low-order twist structures in the western margin of the fault zone, developed in Proterozoic Jinshuikou (Ptjn), Upper Ordovician Darth (O_3ts), Upper Devonian Qisuqun (D_3qg ~ b) and the Valsalva intrusive rocks. Four large-scale arc-shaped faults are scattered around the core block of Khalkhansan Mountains to the east and south, forming a relatively complete broom image see Attachment).