Study on Dynamic Characteristics of Crustal Deformation in the Yunnan Area Using GPS

【摘要】 Based on the GPS velocity field data of 1999-2007 and 2011-2013,we used the least squares configuration method and GPS velocity profile results to synthetically analyze the dynamic evolution characteristics of crustal deformation in the Yunnan area before and after the Wenchuan earthquake. The dynamic evolution of GPS velocity field shows that the direction is gradually changed from the south in the southern part of the SichuanYunnan block to the south-west in the southern Yunnan block and there is a clear relative motion characteristic near the block boundary fault zone. Compared with the GPS velocity of 1999-2007,the results of 2011-2013 also reflect segmental deformation characteristics of the block boundary fault zone. Southeast movement shows a significant increase,which may be related to crustal deformation adjustment after the Wenchuan earthquake. The dynamic evolution of strain parameters shows a pattern of"extension in the middle and compression at both ends"in the whole area and the distribution of deformation(shear,extension or compression)is closely related to the background motion and deformation characteristics of the main fault zone. Compared with the results of the period of 1999-2007,the extensional deformation zone of 2011-2013 is expanded eastward and southward. The compressional deformation of the eastern boundary(the Xiaojiang fault zone)of the Sichuan-Yunnan block is no longer significant,which is mainly concentrated in the northern section of the Xiaojiang fault zone and may be related to the post-seismic deformation adjustment of the Wenchuan earthquake. The GPS velocity profile results show that the left-lateral slip velocity of the Xiaojiang fault zone reduced gradually from north to south(10 mm/a-5 mm/a),and the width of the northern section is wider. The right-lateral slip rate of the Honghe fault zone is about 4 mm/a,and the deformation width is wider. The dynamic results show that the Wenchuan earthquake has little effect on the deformation modes of these two fault zones.更多还原

【Abstract】 Based on the GPS velocity field data of 1999-2007 and 2011-2013,we used the least squares configuration method and GPS velocity profile results to synthetically analyze the dynamic evolution characteristics of crustal deformation in the Yunnan area before and after the Wenchuan earthquake. The dynamic evolution of GPS velocity field shows that the direction is gradually changed from the south in the southern part of the SichuanYunnan block to the south-west in the southern Yunnan block and there is a clear relative motion characteristic near the block boundary fault zone. Compared with the GPS velocity of 1999-2007,the results of 2011-2013 also reflect segmental deformation characteristics of the block boundary fault zone. Southeast movement shows a significant increase,which may be related to crustal deformation adjustment after the Wenchuan earthquake. The dynamic evolution of strain parameters shows a pattern of"extension in the middle and compression at both ends"in the whole area and the distribution of deformation(shear,extension or compression)is closely related to the background motion and deformation characteristics of the main fault zone. Compared with the results of the period of 1999-2007,the extensional deformation zone of 2011-2013 is expanded eastward and southward. The compressional deformation of the eastern boundary(the Xiaojiang fault zone)of the Sichuan-Yunnan block is no longer significant,which is mainly concentrated in the northern section of the Xiaojiang fault zone and may be related to the post-seismic deformation adjustment of the Wenchuan earthquake. The GPS velocity profile results show that the left-lateral slip velocity of the Xiaojiang fault zone reduced gradually from north to south(10 mm/a-5 mm/a),and the width of the northern section is wider. The right-lateral slip rate of the Honghe fault zone is about 4 mm/a,and the deformation width is wider. The dynamic results show that the Wenchuan earthquake has little effect on the deformation modes of these two fault zones.更多还原