青藏块体东北缘地壳水平运动状态
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摘要
应用青藏块体东北缘 1999~ 2 0 0 3年多期GPS观测资料 ,计算了不同时段GPS点水平运动速率。通过分析发现 :甘青块体可分为东部块体和西部块体 ,东、西部块体的运动状态存在明显的差异 ;受 2 0 0 1年 11月 14日昆仑Ms8.1地震的影响 ,震后地壳运动状态发生了明显的改变
In this paper,we have calculated the horizontal movement rate of GPS sites in northeastern margin of the Qinghai Tibet block by use of GPS observing data from 1999 to 2003.It is found that Gan Qing block can be divided into west block and east block,and there is a explicit difference of movement state between the two blocks.By the influence of Kunlun 8.1 earthquake on Nov. 14,2001,the state of horizontal movement has changed explicitly after the earthquake.
引文
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