昆仑山脉中、东段横亘在青海省中部,北临柴达木盆地,南与乌丽—可可西里中新生代盆地和巴颜喀拉山及扎莫吐新生代盆地毗邻(图1)。挽近时间内,在华力西地槽褶皱带的基础上,昆仑褶皱带块体以巨大的速度隆升,造就了当今举世瞩目的“莽昆仑”。然而从新构造运动的实质剖析,它是一座以特殊的掀斜运动形式所形成的倾斜山系。 In the middle of the Kunlun Mountains, the eastern segment runs through the central Qinghai Province, to the north of the Qaidam Basin, to the south of the Wu Li-Hoh Xil Mesozoic basin and to the Bayan Har Mountains and the Zamormu Cenozoic basin (Figure 1). In recent times, on the basis of the crustal belt of the Variscan trough, the Kunlun fold belt blocks have risen at a tremendous speed, creating the “Mang Kunlun” that attracts worldwide attention. However, from the real analysis of the new tectonic movement, it is a sloped mountain system formed by a special tilting movement.