Characteristics of current crustal movement in Qinghai-Tibetan Plateau were analyzed with least square collusion and wavelet using GPS data, and crustal movement strength and vortex movement were analyzed quantitatively. The conclusions are drawn as follows: The crustal movement strength in Qinghai-Tibetan Plateau decreases from west to east along arc tectonic ruptures formed by Kala-Kunlun, Mani, Yushu, Xianshuihe and Xiaojiang faults. The crustal movement strengths in north and west are stronger than those of south and east in the Sichuan-Yunnan block, of which east boundaries are obvious, and west boundaries are not.