Based on geomorphological, tectonic and sedimentary data, a Kunlun Yel
low River Tectonic Movement has been recognized in 1.10-0.60 Ma B.P. T
his tectonic movement, which leads to uplift of the Qinghai-Xizang (Ti
bet) plateau from 1500 to 3000-3500 m, is periodic, abrupt and changea
ble in the movement rate of uplifting and slide slipping.