Current horizontal strain field in Chinese mainland derived from GPS data

2002 ◽  
Vol 15 (4) ◽  
pp. 351-362 ◽  
Author(s):  
Guo-hua Yang ◽  
Yan-xing Li ◽  
Yue-ping Han ◽  
Xin-kang Hu ◽  
Yue-mu Gong
2004 ◽  
Vol 47 (2) ◽  
pp. 245-257 ◽  
Author(s):  
Yan-Xing LI ◽  
Zhi LI ◽  
Jing-Hua ZHANG ◽  
Cheng HUANG ◽  
Wen-Yao ZHU ◽  
...  

1998 ◽  
Vol 11 (4) ◽  
pp. 403-412 ◽  
Author(s):  
Shuo-Yu Zhou ◽  
Yue-Gang Zhang ◽  
Guo-Yu Ding ◽  
Yun Wu ◽  
Xiao-Jun Qin ◽  
...  

2008 ◽  
Vol 21 (6) ◽  
pp. 562-572
Author(s):  
Liang-qian Guo ◽  
Yan-xing Li ◽  
Guo-hua Yang ◽  
Xin-kang Hu

2006 ◽  
Vol 19 (5) ◽  
pp. 514-521
Author(s):  
Shao-qun Jing ◽  
Jia-wei Wang ◽  
Yun Wu ◽  
Shuo-yu Zhou ◽  
Shun-ying Shi

1999 ◽  
Vol 12 (5) ◽  
pp. 596-606 ◽  
Author(s):  
Yun Wu ◽  
Ping Shuai ◽  
Shuo-Yu Zhou ◽  
Xiao-Jun Qin ◽  
Shun-Ying Shi ◽  
...  

2013 ◽  
Vol 353-356 ◽  
pp. 3464-3467
Author(s):  
Yong Sheng Chen ◽  
Qun He ◽  
Jun Yu Chen ◽  
Hong Bin Ma

By using all 103 days GPS data of IGS in china, from year 2000 to 2005, the baseline is solved with GSMIT software. With One day's baseline solution as the input data, based on the mathematical floating model of station, the floating velocity of station is solved and the crustal movement is gotten; then, according to Euler theorem of plate movement, the Euler vectors of Chinese mainland is obtained; furthermore, the floating velocity of the station area in Eurasian plate is acquired. The results show that, in ITRF2000 framework, the station floating velocity is similar with what announced by IGS and so does the Euler vector, which shows that the continental shelf of China has an accelerated tendency to eastward movement.


2015 ◽  
Vol 6 (1) ◽  
pp. 7-15 ◽  
Author(s):  
Bin Zhao ◽  
Yong Huang ◽  
Caihong Zhang ◽  
Wei Wang ◽  
Kai Tan ◽  
...  

2016 ◽  
Vol 73 (7) ◽  
pp. 2837-2850 ◽  
Author(s):  
Callum J. Shakespeare

Abstract A simple analytical model is developed to describe wave generation during frontogenesis forced by a horizontal strain field. In contrast to previous models, neither geostrophic nor hydrostatic balance is assumed. The generated waves are trapped in the strain field and form steady bands of enhanced vertical flow on either side of the surface front on scales from 1 to 100 km. The predictions of the analytical model are confirmed by comparison with fully nonlinear numerical simulations.


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