基于中国地壳运动观测网络区域网1999--2011年六期GPS数据和中国大陆构造环境监测网络2009—2011年区域网部分测站的两期观测数据,利用BERNESE软件解算了测站的位移速率,给出了测站水平运动和垂直运动的速度场。初步结果表明中国大陆大部分地区的地壳垂直运动速率较低,其中青藏高原地区地壳垂直运动趋势整体表现为较低速率的隆升。
Using campaign - mode GPS data of 6 periods from Crustal Movement Observation Network of China surveyed in 1999 -2011 and data of 2 periods from Continental Tectonic Environment Monitoring Network of China surveyed in 2009 -2011 we derive the movement rates of these stations. Both horizontal and vertical velocity fields in the Chinese mainland have been calculated with BERNESE GPS software. Preliminary results of the vertical ve- locity field demonstrate that the general trend of Tibetan Plateau is up with low rates.