Using repeated precise gps campaigns for research of present-day crustal movement and strain in the Qinghai-Tibetan Plateau
Chinese Science Bulletin Vol. 46 No.8 April 2001，-0001，（）：
of the Tibet block relative to Golmud in the north and south directions is (9.3±4.6)mm/a, the strain velocity of the middle part in the west and east directions is (15.6±6.3)mm/a, reflecting the plateau lateral extruding movement. The Himalayan block is mainly compressing strain, and the middle part of the Tibet block is mainly extending strain. The highest extending and the compressing strain are 0.131×10−6/a and −0.189×10−6/a, respectively.
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