摘要
///Based on GNSS observation (from 1999 to 2007, and from 2009 to 2010) and continuous variation of deformation field, this study employed filtering and analysis of multi-kernel function and an unbiased algorithm of strain field to obtain movement and deformation field of the southeastern of Qinghai-Tibetan Plateau before and after the MS7.1 Yushu and MS8.0 Wenchuan earthquakes. The observations showed:1) tectonic activities of seismic source were significantly weakened at spatial and relative long time level before the Yushu and Wenchuan earthquake; 2) spin shear deformation corresponding to the earthquake rupture was neither in nor far from the seismic source region, and there seemed an orderly coordinated action; 3) the trange of large co-seismic horizontal deformation of the Yushu earthquake was actually small; and 4) the North and the surrounding of Litang-Dewu fault zone should be given more attentions.