摘要
In a unified framework, the authors calculate the selected GPS data in South Tianshan area of Xinjiang from 2005 to 2009, and illustrate the principal strain, the shear strain, and the change rate of baseline in different periods to study the crustal movement in this area. The authors find that the crustal deformation in this area is decreasing both from west to east and from south to north, and the principal compressive strain features a compressive stress field in a nearly South-North direction, which results from the northward pushing of the Indian Plate. Then, according to the change rate of the baseline, the authors find that the south part is fiercely compressed by the Tarim Block and the Qinghai-Tibetan Plateau,and the crustal movement in the south of Kashi is relatively active.